华北克拉通中东部典型地区橄榄岩捕虏体年龄及地幔不均一性
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摘要
华北克拉通东部显生宙岩石圈破坏及其深部过程研究是我国固体地球科学的重要议题。在经历了中生代岩石圈减薄之后，地幔的性质和时代等对于认识华北克拉通岩石圈自古生代以来的演化历史及约束减薄机制都具有十分重要的意义。论文选择位于华北克拉通内部造山带北缘的汉诺坝、东部郯庐断裂带上昌乐—山旺以及位处南北重力梯度带上的鹤壁地区新生代玄武岩中的橄榄岩捕虏体作为研究对象，通过详细的岩石学、地球化学和Re-Os同位素年代学的对比研究，获得了以下的主要认识：
1．汉诺坝橄榄岩捕虏体以二辉橄榄岩为主，有少量方辉橄榄岩(Cpx＜5％)；昌乐—山旺地区幔源捕虏体则仅见二辉橄榄岩，单斜辉石含量相对较高；鹤壁捕虏体以粗粒方辉橄榄岩为主，少量二辉橄榄岩。二辉橄榄岩矿物组合为橄榄石+斜方辉石+单斜辉石±尖晶石，方辉橄榄岩矿物组合为橄榄石+斜方辉石±单斜辉石±尖晶石。
2．对比了橄榄岩捕虏体的矿物主量元素和单斜辉石微量元素。汉诺坝橄榄石的Mg~#为86．4-92．8，较该区已发表的分析结果变化范围宽，Mg~#最高值与鹤壁难熔橄榄岩中者相当，方辉橄榄岩中橄榄石Mg~#大于二辉橄榄岩；山旺橄榄岩捕虏体中橄榄石的Mg~#变化范围集中于80．2-90．9之间；鹤壁橄榄石Mg~#则以＞92为主。各地区单斜辉石和尖晶石中Mg~#-Cr~#关系表明鹤壁橄榄岩难熔程度最高，山旺橄榄岩则相对饱满，而汉诺坝橄榄岩则体现了该区岩石圈地幔从饱满到难熔的“混杂”属性。各区橄榄岩捕虏体中微量元素丰度有差异，但单斜辉石微量元素都具有富集Th、U以及亏损高场强元素Nb、Ti、Zr和Hf的特点。稀土元素配分型式上，各区都有LREE富集型和亏损型两种配分型式，体现了研究区陆下岩石圈地幔演化过程中部分熔融和受到熔／流体的交代作用特征。计算了橄榄岩的平衡温度，与橄榄石的Mg~#值之间无相关性。
3．橄榄岩捕虏体的主量元素中岩石难熔程度的指标(如Mg／Si、Mg~#及Al_2O_3+CaO等)显示出汉诺坝捕虏体橄榄岩体现出的特点是既有难熔程度较高，与鹤壁橄榄岩捕虏体接近的样品，也有相对饱满，与昌乐—山旺大部分样品特征一致的橄榄岩。全岩与单斜辉石中微量元素反映的信息较为一致。相容元素与MgO的相关性较好，不相容元素与MgO之间的相关性普遍较差，反映地幔橄榄岩可能经历了较为复杂的部分熔融和后期交代过程。
4．对研究区部分熔融程度和交代作用介质进行了定性、定量的分析判断。昌乐—山旺橄榄岩所代表的岩石圈地幔是经过较低程度熔融抽取后形成的(1％-5％)，后期主要受到硅酸盐熔体的交代作用，具有富集地幔特征；鹤壁是经历了原始地幔高度熔融(15％-20％)抽取后的具有难熔亏损性质的古老岩石圈地幔，后期经历过碳酸岩熔体的强烈改造；汉诺坝地区表现为不同部分熔融程度抽取后的亏损地幔(15％-20％)和富集地幔(＜5％)共存，兼有过渡类型(5％-10％)，在交代介质上以硅酸盐熔体交代为主，并同时有碳酸岩熔体交代的痕迹。
5．对汉诺坝中包裹体硫化物和填隙状硫化物做了原位的Re-Os同位素分析，并同时分析了汉诺坝和昌乐橄榄岩全岩中Re-Os同位素特征加以对比研究。硫化物较全岩更宽的Re-Os同位素比值范围说明全岩可能中和了不同产状、不同成因的硫化物的Re-Os同位素。汉诺坝橄榄岩捕虏体中硫化物提供了太古代—早元古代(1．8-2．3Ga)—中元古代(0．9-1．4Ga)—晚元古代(0．6Ga)的年龄时段，反映了汉诺坝地区岩石圈地幔存在多发事件，也说明了硫化物原位Re-Os同位素定年在揭示岩石圈地幔演化细节上的优势。昌乐地区橄榄岩全岩给出的最老T_(RD)模式年龄为1．2Ga，Os代理等时线年龄为早元古代的2．1Ga，结合昌乐大多数橄榄岩所具有的新生饱满、富集的特征推断，岩石圈地幔不均一性可能在华北陆下普遍存在。鹤壁橄榄岩捕虏体中橄榄石内硫化物提供了古老太古代(2．5Ga和3．0Ga)年龄，说明了该区仍然残存了古老岩石圈地幔。
6．对华北克拉通中、东部新生代时岩石圈地幔的不均一性进行了探讨，并提出了新生代岩石圈地幔演化过程。自东向西由昌乐—山旺、鹤壁和汉诺坝橄榄岩捕虏体代表的新生代时华北克拉通岩石圈地幔在岩石类型、结构、化学成分、熔融抽取程度、交代介质以及Re-Os同位素特征和年龄结构上存在明显的不均一性特征。这种地幔不均一性最好的解释应该是华北东部岩石圈经历了上涌软流圈物质通过侵蚀、混合和改造实现了对古老岩石圈地幔的不均匀置换，并从而实现了华北东部岩石圈的巨厚减薄。就现有地幔年龄数据来看，华北东部古老太古代岩石圈在早元古代时(1．9-2．3Ga)发生了一次大规模的置换作用，将昌乐—山旺古老岩石圈地幔完全置换，但在鹤壁代表的克拉通南部和汉诺坝所代表的西部地区仅体现了不均匀的置换，因而在这些地区仍然残留了较老的岩石圈地幔。在之后的中、晚元古代汉诺坝地区岩石圈地幔又经历了多次深部热事件作用过程(1．2-1．4Ga，0．6-0．9Ga)，但未受中生代华北克拉通东部岩石圈巨厚减薄的影响。早元古代被完全置换的昌乐—山旺岩石圈地幔受中生代形成的郯庐断裂带影响，在中生代岩石圈减薄作用过程中，较易被置换改造，因此其地幔主体表现为新生特点，其个别样品异常高的Re含量和高于原始的Re-Os同位素比值也可以说明昌乐—山旺岩石地幔较新，但新生物质对古老地幔的不均匀置换使得昌乐—山旺地区可能仍保留了一部分元古代岩石圈地幔。
The Phanerozoic considerable losing of the Archean keels of the North China lithospherehave attracted many attentions in the past few years.The nature and age of the North Chinalithospheric mantle are especially important to understand the thinning mechanism and evolutionof the lithosphere.Peridotite xenoliths entrained in the Cenozoic basalts from the North ChinaCraton are ideal samples for investigating the nature and evolution of the lithospheric mantle.Inthis paper,we present detailed petrologic,geochemical and Re-Os geochronologicalinvestigations for the peridotite xenoliths captured in the Cenozoic alkaline basalts fromHannuoba (northern edge of the Trans-North China Orogen within the craton),Changle-Shanwang and Hebi (interior of the craton),with the aim of constraining the age andnature of lithospheric mantle beneath these areas.Our main conclusions are listed as below:
1.The Hannuoba peridotite xenoliths are mainly lherzolites with minor harzburgites (withClinopyroxene content less than 5%);the Changle-Shanwang mantle-derived xenoliths are allmost lherzolites and characterized by high proportion of Clinopyroxene;the Hebi xenoliths aremainly comprised of coarse-grained harzburgites and minor lherzolites.The lherzolites xenolithshave mineral assemblage of olivine+orthopyroxene+Clinopyroxene±Spinel,whereas theharzburgites are characterized by occurrence of olivine+ orthopyroxene±Clinopyroxene±Spinel.
2.The olivine Mg~# of the Harmuoba xenoliths range from 86.4 to 92.8,which are slightlywider than the published data for this area.The highest olivine Mg~# of the Hannuoba samples issimilar to that of the Hebi refractory peridotites,which are interpreted as shallow relics of theArchean cratonic mantle;Mg~# of the harzburgites is higher than the lherzolites in the Hannuobaxenoliths.The olivine Mg~# of the Shanwang xenoliths is mainly concentrated in 80.2-90.9.However,the Mg~# of most Hebi olivine is higher than 92.The Mg~# and Cr~# correlation in theclinopyroxene and spinel indicate that the Hebi peridotites are the most refractory and theChangle-Shanwang samples exhibit more fertile characteristics.The Hannuoba peridotites,however,display heterogeneous characteristics,suggesting the co-existence of both refractoryand fertile mantle components underneath this region.The trace element for the studied xenolithshave differences between each other,however,their clinopyroxenes are all characterized byenrichment of Th,U,and depletion of HFSE such as Nb,Ti,Zr and Hf.Xenoliths from all of the studied areas have two distinct REE distribution patterns including LREE enrich type and LREEdepleted type,further indicating a comprehensive melts/fluids metasomatism within thelithospheric mantle beneath the studied areas.The balance temperatures of the peridotites havebeen calculated,which have no relevance with the Mg~# value in olivine.
3.Some major element,such as MgO,Mg~# and (Al_2O_3+CaO) which are commonly regardedas indicator of lithospheric mantle refractory,also reveal that the Hannuoba peridotitic xenolithsdisplay both refractory and fertile characteristics.Among the Hannuoba peridotites,the much morerefractory samples have similar geochemical features to those of the Hebi peridotites,and therelatively fertile xenoliths exhibit nearly consistent characteristics with those of theChangle-Shanwang.The peridotites whole-rock trace element composition is in agreement withthat of the clinopyroxenes,both are characterized by U,Th enrichment and HFSE depletion.Meanwhile,the Shanwang and minor Hannuoba peridotites have positive Sr anomaly.The MgOexhibits excellent liner correlation with the compatible element but relatively weak linercorrelation with the incompatible element,suggesting that the peridotites may have undergonecomplicated modification.
4.The lithospheric mantle beneath Shanwang area is characterized by enriched feature andhas undergone silicate melts metasomatism,such mantle represents a relatively lower partialmelting (1%-5%) residue and mainly comprises of lherzolites.Most of the Hebi peridotitesrepresent refractory Archean relics that have undergone high proportion of melts exaction(15%-20%) and a later stage carbonatitic melts modification.Lithospheric mantle underneath theHannuoba area,however,exhibits heterogeneous feature,that is,with the coexistence of fertilecomponents (＜5%) and refractory mantle(15%-20%) of different melts exaction proportion,andmainly undergone silicate melts metasomatism with minor carbonatitic metasomatism.
5.Re-Os isotope of the sulfides in peridotites and the whole rocks have been analyzed andcontrasted in this paper.The wider range of Re-Os isotopic ratios in sulfides than those in thewhole rock indicates that the Re-Os isotopes have mixed those in sulfides with differentoccurrence and origin.The maximum Re depleted model age (TRD) of the enclosed sulfides inHannuoba peridotitic xenoliths is 2.1 Ga.The enclosed sulfides,with Re-Os isotopic ratios lowerthan primitive mantle,give an isochron age of 2.3±1.2 Ga.However it is Archean era when theisochron line is fitted without the primitive mantle.All of the interstitial sulfides and some of theenclosed sulfides,with higher Re-Os isotopic ratios than primitive mantle,yield an isochron age of645±225 Ma,which might record mantle melt/fluid activity in SCLM in Neoproterozoic.1.3Gaobtained from an interstitial sulfide is interpreted as a thermal event in Mesoproterozoic.Therefore,several periods of the sulfide Re-Os ages in the Cenozoic Hannuoba peridotitic xenolithssuccessfully reveal the frequently-occurring mantle events and thus complex evolution oflithosphere beneath the North China Block.The oldest TRD age calculated by the Re-Os isotopes inperidotitic xenoliths from Changle is 1.2Ga and the Os proxy isochron is 2.1Ga.Therefore,themantle heterogeneity probably is common beneath the North China Craton according to the fertilecharacters of peridotites from Changle.The Archean age (2.5Ga and 3.0Ga) acquired by the Re-Osisotopes of sulfides in Hebi peridotitic xenoliths implies that the present mantle beneath Hebi is the relic refractory mantle.This mantle heterogeneity is mostly the result of the asthenospheric mantlereplacing the aged craton mantle through erosion,intermingling and modification.
6.The heterogeneous nature of the lithospheric mantle beneath the central and eastern NorthChina Craton has been discussed,and the simply evolutional processes of the lithospheric mantleduring the Cenozoic period have been proposed in this paper.Such lithospheric mantle architectureis consistent with the mantle evolution model that the eastern North China lithospheric mantle hasundergone heterogeneous asthenospheric materials replacement via erosion and modification.Thepresent age data also indicate that the ancient Archean refractory lithospheric mantle beneath theNorth China has undergone a large scale replacement during 2.3-1.9 Ga in the Paleoprotozoic,with shallow relics preserved in Hebi of the central craton and Hannuoba of the northern edge ofthe Trans-North China Orogen within the craton.This is supported by the geochemical data of theperidotites xenoliths.The Hannuoba lithospheric mantle have undergone frequently occurred deepmantle thermal modification at 1.4-1.2 Ga and 0.9-0.6 Ga in the follow Mesoproterozoic andNeoproterozoic periods,but not affected by the considerable lithospheric mantle replacementunderneath the eastern North China Craton during Phanerozoic.Lithospheric mantle beneathChangle-Shanwang area within the Tanlu big fault has undergone at least two stages of mantlereplacement happened the Paleoprotozoic and Mesozoic.The Tanlu big fault provided a prefectway for the asthenospheric materials upwelling,through which finally replaced the Paleoprotozoiclithospheric mantle underneath Changle-Shanwang area and given formation of a newly accretedfertile mantle,with only minor Proterozoic mantle components preserved.This conclusion ispartly supported by the whole-rock Re-Os isotopic data.
1．汉诺坝橄榄岩捕虏体以二辉橄榄岩为主，有少量方辉橄榄岩(Cpx＜5％)；昌乐—山旺地区幔源捕虏体则仅见二辉橄榄岩，单斜辉石含量相对较高；鹤壁捕虏体以粗粒方辉橄榄岩为主，少量二辉橄榄岩。二辉橄榄岩矿物组合为橄榄石+斜方辉石+单斜辉石±尖晶石，方辉橄榄岩矿物组合为橄榄石+斜方辉石±单斜辉石±尖晶石。
2．对比了橄榄岩捕虏体的矿物主量元素和单斜辉石微量元素。汉诺坝橄榄石的Mg~#为86．4-92．8，较该区已发表的分析结果变化范围宽，Mg~#最高值与鹤壁难熔橄榄岩中者相当，方辉橄榄岩中橄榄石Mg~#大于二辉橄榄岩；山旺橄榄岩捕虏体中橄榄石的Mg~#变化范围集中于80．2-90．9之间；鹤壁橄榄石Mg~#则以＞92为主。各地区单斜辉石和尖晶石中Mg~#-Cr~#关系表明鹤壁橄榄岩难熔程度最高，山旺橄榄岩则相对饱满，而汉诺坝橄榄岩则体现了该区岩石圈地幔从饱满到难熔的“混杂”属性。各区橄榄岩捕虏体中微量元素丰度有差异，但单斜辉石微量元素都具有富集Th、U以及亏损高场强元素Nb、Ti、Zr和Hf的特点。稀土元素配分型式上，各区都有LREE富集型和亏损型两种配分型式，体现了研究区陆下岩石圈地幔演化过程中部分熔融和受到熔／流体的交代作用特征。计算了橄榄岩的平衡温度，与橄榄石的Mg~#值之间无相关性。
3．橄榄岩捕虏体的主量元素中岩石难熔程度的指标(如Mg／Si、Mg~#及Al_2O_3+CaO等)显示出汉诺坝捕虏体橄榄岩体现出的特点是既有难熔程度较高，与鹤壁橄榄岩捕虏体接近的样品，也有相对饱满，与昌乐—山旺大部分样品特征一致的橄榄岩。全岩与单斜辉石中微量元素反映的信息较为一致。相容元素与MgO的相关性较好，不相容元素与MgO之间的相关性普遍较差，反映地幔橄榄岩可能经历了较为复杂的部分熔融和后期交代过程。
4．对研究区部分熔融程度和交代作用介质进行了定性、定量的分析判断。昌乐—山旺橄榄岩所代表的岩石圈地幔是经过较低程度熔融抽取后形成的(1％-5％)，后期主要受到硅酸盐熔体的交代作用，具有富集地幔特征；鹤壁是经历了原始地幔高度熔融(15％-20％)抽取后的具有难熔亏损性质的古老岩石圈地幔，后期经历过碳酸岩熔体的强烈改造；汉诺坝地区表现为不同部分熔融程度抽取后的亏损地幔(15％-20％)和富集地幔(＜5％)共存，兼有过渡类型(5％-10％)，在交代介质上以硅酸盐熔体交代为主，并同时有碳酸岩熔体交代的痕迹。
5．对汉诺坝中包裹体硫化物和填隙状硫化物做了原位的Re-Os同位素分析，并同时分析了汉诺坝和昌乐橄榄岩全岩中Re-Os同位素特征加以对比研究。硫化物较全岩更宽的Re-Os同位素比值范围说明全岩可能中和了不同产状、不同成因的硫化物的Re-Os同位素。汉诺坝橄榄岩捕虏体中硫化物提供了太古代—早元古代(1．8-2．3Ga)—中元古代(0．9-1．4Ga)—晚元古代(0．6Ga)的年龄时段，反映了汉诺坝地区岩石圈地幔存在多发事件，也说明了硫化物原位Re-Os同位素定年在揭示岩石圈地幔演化细节上的优势。昌乐地区橄榄岩全岩给出的最老T_(RD)模式年龄为1．2Ga，Os代理等时线年龄为早元古代的2．1Ga，结合昌乐大多数橄榄岩所具有的新生饱满、富集的特征推断，岩石圈地幔不均一性可能在华北陆下普遍存在。鹤壁橄榄岩捕虏体中橄榄石内硫化物提供了古老太古代(2．5Ga和3．0Ga)年龄，说明了该区仍然残存了古老岩石圈地幔。
6．对华北克拉通中、东部新生代时岩石圈地幔的不均一性进行了探讨，并提出了新生代岩石圈地幔演化过程。自东向西由昌乐—山旺、鹤壁和汉诺坝橄榄岩捕虏体代表的新生代时华北克拉通岩石圈地幔在岩石类型、结构、化学成分、熔融抽取程度、交代介质以及Re-Os同位素特征和年龄结构上存在明显的不均一性特征。这种地幔不均一性最好的解释应该是华北东部岩石圈经历了上涌软流圈物质通过侵蚀、混合和改造实现了对古老岩石圈地幔的不均匀置换，并从而实现了华北东部岩石圈的巨厚减薄。就现有地幔年龄数据来看，华北东部古老太古代岩石圈在早元古代时(1．9-2．3Ga)发生了一次大规模的置换作用，将昌乐—山旺古老岩石圈地幔完全置换，但在鹤壁代表的克拉通南部和汉诺坝所代表的西部地区仅体现了不均匀的置换，因而在这些地区仍然残留了较老的岩石圈地幔。在之后的中、晚元古代汉诺坝地区岩石圈地幔又经历了多次深部热事件作用过程(1．2-1．4Ga，0．6-0．9Ga)，但未受中生代华北克拉通东部岩石圈巨厚减薄的影响。早元古代被完全置换的昌乐—山旺岩石圈地幔受中生代形成的郯庐断裂带影响，在中生代岩石圈减薄作用过程中，较易被置换改造，因此其地幔主体表现为新生特点，其个别样品异常高的Re含量和高于原始的Re-Os同位素比值也可以说明昌乐—山旺岩石地幔较新，但新生物质对古老地幔的不均匀置换使得昌乐—山旺地区可能仍保留了一部分元古代岩石圈地幔。
The Phanerozoic considerable losing of the Archean keels of the North China lithospherehave attracted many attentions in the past few years.The nature and age of the North Chinalithospheric mantle are especially important to understand the thinning mechanism and evolutionof the lithosphere.Peridotite xenoliths entrained in the Cenozoic basalts from the North ChinaCraton are ideal samples for investigating the nature and evolution of the lithospheric mantle.Inthis paper,we present detailed petrologic,geochemical and Re-Os geochronologicalinvestigations for the peridotite xenoliths captured in the Cenozoic alkaline basalts fromHannuoba (northern edge of the Trans-North China Orogen within the craton),Changle-Shanwang and Hebi (interior of the craton),with the aim of constraining the age andnature of lithospheric mantle beneath these areas.Our main conclusions are listed as below:
1.The Hannuoba peridotite xenoliths are mainly lherzolites with minor harzburgites (withClinopyroxene content less than 5%);the Changle-Shanwang mantle-derived xenoliths are allmost lherzolites and characterized by high proportion of Clinopyroxene;the Hebi xenoliths aremainly comprised of coarse-grained harzburgites and minor lherzolites.The lherzolites xenolithshave mineral assemblage of olivine+orthopyroxene+Clinopyroxene±Spinel,whereas theharzburgites are characterized by occurrence of olivine+ orthopyroxene±Clinopyroxene±Spinel.
2.The olivine Mg~# of the Harmuoba xenoliths range from 86.4 to 92.8,which are slightlywider than the published data for this area.The highest olivine Mg~# of the Hannuoba samples issimilar to that of the Hebi refractory peridotites,which are interpreted as shallow relics of theArchean cratonic mantle;Mg~# of the harzburgites is higher than the lherzolites in the Hannuobaxenoliths.The olivine Mg~# of the Shanwang xenoliths is mainly concentrated in 80.2-90.9.However,the Mg~# of most Hebi olivine is higher than 92.The Mg~# and Cr~# correlation in theclinopyroxene and spinel indicate that the Hebi peridotites are the most refractory and theChangle-Shanwang samples exhibit more fertile characteristics.The Hannuoba peridotites,however,display heterogeneous characteristics,suggesting the co-existence of both refractoryand fertile mantle components underneath this region.The trace element for the studied xenolithshave differences between each other,however,their clinopyroxenes are all characterized byenrichment of Th,U,and depletion of HFSE such as Nb,Ti,Zr and Hf.Xenoliths from all of the studied areas have two distinct REE distribution patterns including LREE enrich type and LREEdepleted type,further indicating a comprehensive melts/fluids metasomatism within thelithospheric mantle beneath the studied areas.The balance temperatures of the peridotites havebeen calculated,which have no relevance with the Mg~# value in olivine.
3.Some major element,such as MgO,Mg~# and (Al_2O_3+CaO) which are commonly regardedas indicator of lithospheric mantle refractory,also reveal that the Hannuoba peridotitic xenolithsdisplay both refractory and fertile characteristics.Among the Hannuoba peridotites,the much morerefractory samples have similar geochemical features to those of the Hebi peridotites,and therelatively fertile xenoliths exhibit nearly consistent characteristics with those of theChangle-Shanwang.The peridotites whole-rock trace element composition is in agreement withthat of the clinopyroxenes,both are characterized by U,Th enrichment and HFSE depletion.Meanwhile,the Shanwang and minor Hannuoba peridotites have positive Sr anomaly.The MgOexhibits excellent liner correlation with the compatible element but relatively weak linercorrelation with the incompatible element,suggesting that the peridotites may have undergonecomplicated modification.
4.The lithospheric mantle beneath Shanwang area is characterized by enriched feature andhas undergone silicate melts metasomatism,such mantle represents a relatively lower partialmelting (1%-5%) residue and mainly comprises of lherzolites.Most of the Hebi peridotitesrepresent refractory Archean relics that have undergone high proportion of melts exaction(15%-20%) and a later stage carbonatitic melts modification.Lithospheric mantle underneath theHannuoba area,however,exhibits heterogeneous feature,that is,with the coexistence of fertilecomponents (＜5%) and refractory mantle(15%-20%) of different melts exaction proportion,andmainly undergone silicate melts metasomatism with minor carbonatitic metasomatism.
5.Re-Os isotope of the sulfides in peridotites and the whole rocks have been analyzed andcontrasted in this paper.The wider range of Re-Os isotopic ratios in sulfides than those in thewhole rock indicates that the Re-Os isotopes have mixed those in sulfides with differentoccurrence and origin.The maximum Re depleted model age (TRD) of the enclosed sulfides inHannuoba peridotitic xenoliths is 2.1 Ga.The enclosed sulfides,with Re-Os isotopic ratios lowerthan primitive mantle,give an isochron age of 2.3±1.2 Ga.However it is Archean era when theisochron line is fitted without the primitive mantle.All of the interstitial sulfides and some of theenclosed sulfides,with higher Re-Os isotopic ratios than primitive mantle,yield an isochron age of645±225 Ma,which might record mantle melt/fluid activity in SCLM in Neoproterozoic.1.3Gaobtained from an interstitial sulfide is interpreted as a thermal event in Mesoproterozoic.Therefore,several periods of the sulfide Re-Os ages in the Cenozoic Hannuoba peridotitic xenolithssuccessfully reveal the frequently-occurring mantle events and thus complex evolution oflithosphere beneath the North China Block.The oldest TRD age calculated by the Re-Os isotopes inperidotitic xenoliths from Changle is 1.2Ga and the Os proxy isochron is 2.1Ga.Therefore,themantle heterogeneity probably is common beneath the North China Craton according to the fertilecharacters of peridotites from Changle.The Archean age (2.5Ga and 3.0Ga) acquired by the Re-Osisotopes of sulfides in Hebi peridotitic xenoliths implies that the present mantle beneath Hebi is the relic refractory mantle.This mantle heterogeneity is mostly the result of the asthenospheric mantlereplacing the aged craton mantle through erosion,intermingling and modification.
6.The heterogeneous nature of the lithospheric mantle beneath the central and eastern NorthChina Craton has been discussed,and the simply evolutional processes of the lithospheric mantleduring the Cenozoic period have been proposed in this paper.Such lithospheric mantle architectureis consistent with the mantle evolution model that the eastern North China lithospheric mantle hasundergone heterogeneous asthenospheric materials replacement via erosion and modification.Thepresent age data also indicate that the ancient Archean refractory lithospheric mantle beneath theNorth China has undergone a large scale replacement during 2.3-1.9 Ga in the Paleoprotozoic,with shallow relics preserved in Hebi of the central craton and Hannuoba of the northern edge ofthe Trans-North China Orogen within the craton.This is supported by the geochemical data of theperidotites xenoliths.The Hannuoba lithospheric mantle have undergone frequently occurred deepmantle thermal modification at 1.4-1.2 Ga and 0.9-0.6 Ga in the follow Mesoproterozoic andNeoproterozoic periods,but not affected by the considerable lithospheric mantle replacementunderneath the eastern North China Craton during Phanerozoic.Lithospheric mantle beneathChangle-Shanwang area within the Tanlu big fault has undergone at least two stages of mantlereplacement happened the Paleoprotozoic and Mesozoic.The Tanlu big fault provided a prefectway for the asthenospheric materials upwelling,through which finally replaced the Paleoprotozoiclithospheric mantle underneath Changle-Shanwang area and given formation of a newly accretedfertile mantle,with only minor Proterozoic mantle components preserved.This conclusion ispartly supported by the whole-rock Re-Os isotopic data.
引文
1.Liu D Y,Nutman A P,Compston W,et al.Remnants of 3800Ma crust in Chinese part of the Sino-Korean craton.Geology,1992,20:339-342
2.Zheng J P,Griffin W L,O'Reilly S Y,et al.3.6Ga lower crust in central China:new evidence on the assembly of the North China Craton.Geology,2004,32:229-232
3.Menzies M A,Fan W M & Zhang M.Paleozoic and Cenozoic lithoprobes and loss of＞120 km of Archaean lithosphere,Sino-Korean Craton,China.In:Prichard H M,Alabaster T,Harris N B W,et al (eds).Magmatic processes and plate tectonics.Geological Society of London,Special Publication no.76.1993,71-78
4.Menzies M A & Xu Y G.Geodynamics of the North China Craton.In:Flower M,Chung S L,Lo C H,et al (eds).Mantle dynamics and plate interactions in East Asia.American Geophysical Union Geodynamics Series no.27.Washington D C,1998,155-165
5.Griffin W L,Zhang A,O'Reilly S Y,et al.Phanerozoic evolution of the lithosphere beneath the Sino-Korean Craton.In:Flower M,Chung S L,Lo C H,et al (eds).Mantle dynamics and plate interactions in East Asia.American Geophysical Union Geodynamics Series no.27.Washington D C,1998,107-126
6.Xu Y G,Menzies M A,Mattey D P,et al.The nature of lithospheric mantle near the Tancheng-Lujiang fault,China:an integration of texture,chemistry and O-isotopes.Chemical Geology,1996,134:67-81
7.Fan W M,Zhang H F,Baker J,et al.On and off the North China Craton:where is the Archean keel? Journal of Petrology,2000,41:933-950
8． 郑建平．中国东部地幔置换作用与中新生代岩石圈减薄．武汉：中国地质大学出版社，1999
9． 邓晋福，赵海玲，莫宣学，等．中国大陆根柱构造-大陆动力学的钥匙．北京：地质出版社，1996，33-34
10．邓晋福，莫宣学，赵海玲，等．中国东部岩石圈根／去根作用与大陆“活化”-东亚型大陆动力学模式研究计划．现代地质，1994，8(3)：349-356
11．邓晋福，苏尚国，赵海玲，等．华北地区燕山期岩石圈减薄的深部过程．地学前缘,2003，10(3)：41-50
12．邓晋福，苏尚国，刘翠，等．关于华北克拉通燕山期岩石圈减薄的机制与过程的讨论：是拆沉，还是热侵蚀和化学交代?地学前缘，2006，13(2)：105-119
13．吴福元，孙德有．中国东部中生代岩浆作用与岩石圈减薄．长春科技大学学报，1999,29(4)：313-318
14．吴福元，葛文春，孙德有，等．中国东部岩石圈减薄研究中的几个问题．地学前缘,2003，10(3)：S1-60
15．吴福元，徐义刚，高山，等．华北岩石圈减薄与克拉通破坏研究的主要学术争论．岩石学报，2008，24(6)：1145-1174
16.Gao S,Rudnick R L,Yuan H L,et al.Recycling lower continental crust in the North China Craton.Nature,2004,432:892-897
17.Gao S,Rudnick R L,Xu W L,et al.Recycling deep cratonic lithosphere and generation of intraplate magmatism in the North China Craton.Earth and Planetary Science Letters,2008,270:41-53
18.Deng J F,Mo X X,Zhao H L,et al.2004.A new model for the dynamic evolution of Chinese lithosphere:‘continental roots-plume tectonics'.Earth-Science Reviews,2004,65:223-275
19.Deng J F,Su S G,Niu Y L,et al.A possible model for the lithospheric thinning of North China Craton:evidence form the Yanshanian (Jura-Cretaceous) magmatism and tectonism.Lithos,2007,96:22-35
20.Xu W L,Gao S,Wang Q H,et al.Mesozoic crustal thickening of the eastern North China craton:Evidence from eclogite xenoliths and petrologic implications.Geology,2006a,34(9):721-724
21.Xu W L,Wang Q H,Wang D Y,et al.Mesozoic adakitic rocks from the Xuzhou-Suzhou area,eastern China:Evidence for partial melting of delaminated lower continental crust.Journal of Asian Earth Sciences,2006b,27:454-464
22.Xu W L,Hergt J M,Gao S,et al.Interaction of adakitic melt-peridotite:implications for the high-Mg~# signature of Mesozoic adakitic rocks in the eastern North China Craton.Earth and Planetary Science Letters,2008,265:123-137
23.Xu Y G.Thermo-tectonic destruction of the Archean lithospheric keel beneath the Sino-Korean Craton in China:evidence,timing and mechanism.Physics and Chemistry of the Earth (A),2001,26(9-10):747-757
24.Xu Y G,Huang X L,Ma J L,et al.Crust-mantle interaction during the tectono-thermal reactivation of the North China Craton:constraints from SHRIMP zircon U-Pb chronology and geochemistry of Mesozoic plutons from western Shandong.Contribution to Mineralogy and Petrology,2004a,147:750-767
25.Zheng J P,O'Reilly S Y,Griffin W L,et al.Nature and evolution of Cenozoic lithospheric mantle beneath Shandong peninsula,Sino-Korean craton.International Geology Review,1998,40:471-499
26.Zheng J P,Griffin W L,O'Reilly S Y,et al.Late Mesozoic-Eocene mantle replacement beneath the eastern North China Craton:evidences from the Paleozoic and Cenozoic peridotite xenoliths.International Geology Review,2005,47:457-472
27.Zheng J P,Griffin,W L,O'Reilly,S Y,et al.Mineral chemistry of peridotites from Paleozoic,Mesozoic and Cenozoic lithosphere:constraints on mantle evolution beneath eastern China.Journal of Petrology,2006,47(11):2233-2256
28.Zheng J P,Griffin W L,O'Reilly S Y,et al.Mechanism and timing of lithospheric modification and replacement beneath the eastern North China Craton:Peridotitic xenoliths from the 100 Ma Fuxin basalts and a regional synthesis.Geochimica et Cosmochimica Acta,2007,71(21):5203-5225
29．张宏福，英基丰，徐平，等．华北中生代玄武岩中地幔橄榄石捕虏晶：对岩石圈地幔置换过程的启示．科学通报，2004，49(8)：784-789
30.Zhang H F,Sun M,Zhou X H,et al.Secular evolution of the lithosphere beneath the eastern North China Craton:Evidence from Mesozoic basalts and high-Mg andesites.Geochimica et Cosmochimica Acta,2003,67(22):4373-4387
31.Zhang H F,Ying J F,Shimoda G,et al.Importance of melt circulation and crust-mantle interaction in the lithospheric evolution beneath the North China Craton:evidence from Mesozoic basalts-borne clinopyroxene xenocrysts and pyroxenite xenoliths.Lithos,2007,96:67-89
32．姜耀辉，蒋少涌，赵葵东，等．辽东半岛煌斑岩SHRIMP锆石U-Pb年龄及其对中国东部岩石圈减薄开始时间的制约．科学通报,2005，50(19)：2161-2168
33．许文良，王冬艳，王清海，等．华北地块中东部中生代侵入杂岩中角闪石和黑云母的~(40)Ar/~(39)Ar定年：对岩石圈减薄时间的制约．地球化学，2004a,33(3)：221-231
34.Wu F Y,Walker R J,Ren X W,et al.Osmium isotopic constraints on the age of lithospheric mantle beneath Northeastern China.Chemical Geology,2003,196:107-129
35.Wu F Y,Lin J Q,Wilde S A,et al.Nature and significance of the Early Cretaceous giant igneous events in eastern China.Earth and Planetary Sciences Letters,2005,233:103-119
36.Zhang H F,Sun M,Zhou X H,et al.Geochemical constraints on the origin of Mesozoic alkaline intrusive complexes from the North China Craton and tectonic implications.Lithos,2005,81:297-317
37．伍家善，耿元生，沈其韩，等．华北陆台早前寒武纪重大地质事件．北京：地质出版社，1991
38．李继亮．五台山早元古代碰撞造山带的初步认识．地质科学，1990，1：1-11
39.Zhao G C,Wilde S A,Cawood P A,et al.Thermal evolution of Archean basement rocks from the eastern part of the Noryh Chian craton and its bearing on tectonic setting.International Geology Review,1998,40:706-721
40.Wang W.Formation of diamond with mineral inclusions of “mixed” eclogite and peridotite paragenesis.Earth and Planetary Science Letters,1998,160:831-843
41．路凤香，韩柱国，郑建平，等．辽宁复县地区古生代岩石圈地幔特征．地质科技情报，1991，10(增)：1-20
42．翟明国，朱日祥，刘建明，等．华北东部构造体制转折的关键时限．中国科学(D辑)，2003，33(10)：913-920
43．徐义刚．华北岩石圈减薄的时空不均一特征．高校地质学报，2004，10(3)：324-331
44．许文良，王清海，王冬艳，等．华北克拉通东部岩石圈减薄的过程与机制：中生代火成岩和深源捕虏体证据．地学前缘，2004b，11(3)：309-317
45．王晓蕊，高山，柳小明，等．辽西四合屯早白垩世义县组高镁安山岩的地球化学：对下地壳拆沉作用和Sr／Y变化的指示．中国科学(D辑)，2005，35(8)：700-709
46.Zhang H F,Sun M,Zhou X H,et al.Mesozoic lithosphere destruction beneath the North China Craton:evidence from major-,trace-element and Sr-Nd-Pb isotope studies of Fangcheng basalts.Contribution to Mineralogy and Petrology,2002,144:241-253
47.Fan W M,Guo F,Wang Y J,et al.Post-Orogenic bimodal volcanism along the Sulu orogenic belt in eastern China.Physics and Chemistry of the Earth (A),2001,26(9-10):733-746
48.Guo F,Fan W M,Wang Y J,et al.Origin of early Cretaceous calc-alkaline lamprophyres from the Sulu orogen in eastern China:implications for enrichment processes beneath continental collisional belt.Lithos,2004,78:291-305
49.Liu S,Hu R Z,Gao S,et al.U-Pb zircon age,geochemical and Sr-Nd-Pb-Hf isotopic constraints on age and origin of alkaline intrusions and associated mafic dikes from Sulu orogenic belt,Eastern China.Lithos,2008a,106:365-379
50.Tang H Y,Zheng J P,Yu C M.Age and composition of the Rushan intrusive complex in the northern Sulu orogen,eastern China:petrogenesis and lithospheric mantle evolution.Geological Magazine,2009,146(2):199-215
51.Xu Y G,Ma J L,Huang X L,et al.Early Cretaceous gabbroic complex from Yinan,Shandong Province:petrogenesis and mantle domains beneath the North China Craton.International Journal of Earth Science,2004b,93:1025-1041
52.Guo F,Fan W M,Wang Y J,et al.Late Mesozoic mafic intrusive complexes in North China Block:constraints on the nature of subcontinental lithospheric mantle.Physics and Chemistry of the Earth (A),2001,26(9-10):759-771
53.Ying J F,Zhou X H,Zhang H F.Geochemical and isotopic investigation of the Laiwu-Zibo carbonatites from western Shandong province,China and implications for their petrogenesis and enriched mantle source.Lithos,2004,75:413-426
54.Ying,J F,Zhou,X H,Zhang H E The geochemical variations of mid-Cretaceous lavas across western Shandong province,China and their tectonic implications.International Journal of Earth Science,2006a,95:68-79
55.Yang J H,Chung S L,Zhai M G,et al.Geochemical and Sr-Nd-Pb isotopic compositions of mafic dikes from the Jiaodong peninsula,China:evidence for vein-plus-peridotite melting in the lithospheric mantle.Lithos,2004,73:145-160
56.Liu S,Hu R Z,Gao S,et al.Zircon U-Pb geochronology and major,trace elemental and Sr-Nd-Pb isotopic geochemistry of mafic dykes in western Shandong Province,eastern China:Constraints on their petrogenesis and geodynamic significance.Chemical Geology,2008b,255:329-345
57．杨进辉，朱美妃，刘伟，等．胶东地区郭家岭花岗闪长岩的地球化学特征及成因．岩石学报，2003，19(4)：692-700
58．袁洪林，柳小明，刘勇胜，等．北京西山晚中生代火山岩U-Pb锆石年代学及地球化学研究．中国科学(D辑)，2005，35(9)：821-836
59．杨承海，许文良，杨德彬，等．鲁西中生代高Mg闪长岩的成因：年代学与岩石地球化学证据．地球科学-中国地质大学学报，2006，31(1)：81-92
60．杨承海，许文良，杨德彬，等．鲁西上峪辉长-闪长岩的成因：年代学与岩石地球化学证据．中国科学(D辑)，2008，38(1)：44-55
61.Chen B,Jahn B M,Arakawa Y,et al.Petrogenesis of the Mesozoic intrusive complexes from the southern Taihang orogen,North China Craton:elemental and Sr-Nd-Pb isotopic constraints.Contribution to Mineralogy and Petrology,2004,148:489-501
62.Chen B,Zhai M G.Geochemistry of late Mesozoic lamprophyre dykes from the Taihang Mountains,North China,and implications for the sub-continental lithospheric mantle.Geological Magazine,2003,140:87-93
63.Chen B,Tian W,Jahn B M,et al.Zircon SHRIMP U-Pb ages and in-situ Hf isotopic analysis for the Mesozoic intrusions in Southern Taihang,North China craton:evidence for hybridization between mantle-derived magmas and crustal components.Lithos,2008,102(1-2):118-137
64.Wang Y J,Fan W M,Zhang H F,et al.Early Cretaceous gabbroic rocks from the Taihang Mountains:implications for a paleosubduction-related lithospheric mantle beneath the central North China Craton.Lithos,2006,86:281-302
65．陈斌，田伟，翟明国，等．太行山和华北其它地区中生代岩浆作用的锆石U-Pb年代学和地球化学特征及其岩浆成因和地球动力学意义．岩石学报，2005，21(1)：13-24
66．陈斌，翟明国，邵济安．太行山北段中生代岩基的成因和意义：主要和微量元素地球化学证据．中国科学(D辑)，2002,32(11)：896-907
67．蔡剑辉，阎国翰，肖成东，等．太行山大兴安岭构造岩浆带中生代侵入岩Nd、sr、Pb同位素特征及物质来源探讨．岩石学报，2004，20(5)：1225-1242
68．彭头平，王岳军，范蔚茗，等．南太行山闪长岩的SHRIMP锆石U-Pb年龄及岩石成因研究．岩石学报，2004，20(5)：1253-1262
69．许文良，王冬艳，高山，等．鲁西中生代金岭闪长岩中纯橄岩和辉石岩包体的发现及其意义．科学通报，2003a，48(8)：863-868
70．许文良，王冬艳，王清海，等．鲁西中生代闪长岩中两类幔源捕虏体的岩石学和地球化学．岩石学报,2003b，19(4)：623-636
71.Zheng J P,Sun M,Zhou M F,et al.Trace elemental and PGE geochemical constraints of Mesozoic and Cenozoic peridotitic xenoliths on lithospheric evolution of the North China Craton.Geochimica et Cosmochimica Acta,2005,69(13):3401-3418
72.Zhang H F,Sun M,Zhou M F,et al.Highly heterogeneous late Mesozoic lithospheric mantle beneath the North China Craton:evidence from Sr-Nd-Pb isotopic systematics of mafic igneous rocks.Geological Magazine,2004,141:55-62
73．张儒媛，从柏林．安徽女山碧玄岩及其榄岩类包体的成因岩石学和大地构造意义．岩石学研究，1983，(3)：111-128
74.Xu X S,O'Reilly S Y,Griffin W L,et al.The nature of the Cenozoic lithosphere beneath Nushan,East Central China.Flower M F J,Chung S L,Lo C H,et al.Mantle Dynamics and Plate Interactions in East Asia.American Geophysical Union,1998,117-138
75.Song Y,Frey F A.Geochemistry of peridotite xenoliths in basalt from Hannuoba,Eastern China:Implications for Subcontinental mantle heterogeneity.Geochimica et Cosmochimica Acta,1989,53:97-113
76.Chen,S H,O'Reilly,S Y,Zhou X H,et al.Thermal and petrological structure of the lithosphere beneath Hannuoba,Sino-Korean Craton,China:evidence from xenoliths.Lithos, 2001,56:267-301
77.Rudnick R L,Gao S,Ling W L,et al.Petrology and geochemistry of spinel peridotite xenoliths from Hannuoba and Qixia,North China craton.Lithos,2004,77:609-637
78．鄂莫岚，路凤香，邓晋福．吉林汪清超镁铁岩包体的岩石学特征及辉石岩成因问题的讨论．地球化学，1982，18：39-56
79．方同辉，马鸿文．辽宁宽甸地区上地幔岩石圈组成及热结构．地质论评，1999，45(增)：450-457
80．路凤香，郑建平．华北地台古生代岩石圈地幔特征及深部过程．见：池际尚，路凤香主编，华北地台金伯利岩及古生代岩石圈地幔特征，北京：科学出版社，1996
81.Zheng J P,O'Reilly S Y,Griffin W L,et al.Relict refractory mantle beneath the eastern North China block:significance for lithosphere evolution.Lithos,2001:57:43-66
82.Gao S,Zhang B R,Jin Z M,et al.How mafic is the lower continental crust? Earth planetary Science Letter,1998,161:101-117
83．路凤香，郑建平，李伍平，等．中国东部显生宙地幔演化的主要样式：“蘑菇云”模型．地学前缘，2000,7(1)：97-107
84．路凤香，郑建平，邵济安，等．华北东部中生代晚期-新生代软流圈上涌与岩石圈减薄．地学前缘,2006，13(2)：86-92
85.Zhang H F.Transformation of lithospheric mantle through peridotite-melt reaction:a case of Sino-Korean craton.Earth and Planetary Science Letters,2005,237:768-780
86．张宏福，周新华，范蔚茗，等．华北东南部中生代岩石圈地幔性质、组成、富集过程及其形成机理．岩石学报，2005，21(4)：1271-1280
87．支霞臣．Re-Os同位素体系和大陆岩石圈地幔定年．科学通报，1999,44(22)：2362-2371
88.Walker R J,Carlson R W,Shirey S B,et al.Os,Sr,Nd and Pb isotope systematics of southern African peridotite xenoliths:implications for the chemical evolution of Subcontinental mantle.Geochimica et Cosmochimica Acta,1989,53:3005-3013
89.Carlson R W,Irving A J.Depletion and enrichment history of subcontinental lithospheric mantle an Os,Sr,Nd and Pb isotopic study of ultramafic xenoliths from the northwestern Wyoming Craton.Earth and Planetary Science Letters,1994,126:457-472
90.Pearson D G,Carlson R W,Shirey S B,et al.The stabilization of Archaean lithospheric mantle:a Re-Os isotope study of peridotite xenoliths from the Kaapvaal and Siberian cratons.Earth and Planetary Science Letters,1995,134:341-357
91.Pearson D G.The age of continental roots.Lithos,1999,48:171-194
92.Shirey S B,Walker R J.The Re-Os isotope system in cosmochemistry and high-temperature geochemistry.Annu.Rev.Earth Planet.Sci.,1998,26:423-500
93.Meisel T,Walker R J,Irving A J,et al.Osmium isotopic compositions of mantle xenoliths:A global perspective.Geochimica et Cosmochimica Acta,2001,65(8):1311-1323
94.Carlson R W.Application of the Pt-Re-Os isotopic systems to mantle geochemistry and geochronology.Lithos,2005,82:249-272
95.Faure G.Principles of Isotope Geology,John Wiley & sons,Inc.,1986,264-268
96.Reisberg L,Lorand J P.Longevity of sub-continental mantle lithosphere from osmium isotope systematics in orogenic peridotite massifs.Nature,1995,376:159-162
97．吴福元，杨进辉，储著银，等．大陆岩石圈地幔定年．地学前缘，2007，14(2)：76-86
98.Schmitz M D,Bowring S A,Wit M J.Subduction and terrane collision stabilize the western Kaapvaal craton tectosphere 2.9 billion years ago.Earth and Planetary Science Letters,2004,222:363-376
99.Irvine G J,Pearson D G,Kjarsgaard B A.A Re-Os isotope and PGE study of kimberlite-derived peridotite xenoliths from Somerset Island and a comparison to the Slave and Kaapvaal cratons.Lithos,2003,71:46t-488
100.Olive V,Ellam R M,Harte B.A Re-Os isotope study of ultramafic xenoliths from the Matsoku kimberlite.Earth and Planetary Science Letters,1997,150:129-140
101.Pearson D G,Snyder G A,Shirey S B,et al.Archean Re-Os age for Siberian eclogites and constrains on Archean tectonics.Nature,1995,374:711-713
102.Peslier A H,Reisberg L,Ludden J,et al.Os isotopic systematics in mantle xenoliths;age constraints on the Canadian Cordillera lithosphere.Chemical Geology,2000,166:85-101
103.Handler M R,Wysoczanski R J,Gamble J A.Proterozoic lithosphere in Marie Byrd Land,West Antarctica:Re-Os systematics of spinel peridotite xenoliths.Chemical Geology,2003,196:131-145
104.Lee S R,Walker R J.Re-Os isotope systematics of mantle xenoliths from South Korea:evidence for complex growth and loss of lithospheric mantle beneath East Asia.Chemical Geology,2006,231:90-101
105.Schilling M E,Carlson R W,Conceic~o R V.Re-Os isotope constraints on subcontinental lithospheric mantle evolution of southern South America.Earth and Planetary Science Letters,2008,268:89-101
106.Burnham O M,Rogers N W,Pearson D G,et al.The petrogenesis of the eastern Pyrenean peridotites:An integrated study of their whole-rock geochemistry and Re-Os isotope composition.Geochimica et Cosmochimica Acta,1998,62(13):2293-2310
107.Reisberg L,Allegre C J,Luck J M.The Re-Os systematics of Ronda ultramafic complex of southern Spain.Earth and Planetary Science Letters,1991,105:196-219
108.Roy-Barman M,Allegre C J.~(187)Os/~(186)Os ratios of mid-ocean ridge basalts and abyssal peridotites.Geochimica et Cosmochimica Acta,1994,(58):5043-5054
109.Meisel T,Walker R J,Morgen J W.The osmium isotopic composition of the Earth's primitive upper mantle.Nature,1996,383:517-520
110.Meisel T,Melcher F,Tomascak P,et al.Re-Os isotopes in orogenic peridotite massifs in the Eastern Alps,Austria.Chemical Geology,1997,143:217-229
111.Harvey J,Garmoun A,Burton K W,et al.Ancient melt extraction from the oceanic upper mantle revealed by Re-Os isotopes in abyssal peridotites from the Mid-Atlantic ridge.Earth and Planetary Science Letters,2006,244:606-621
112.Tessalina S G,Bourdon B,Gannoun A,et al.Complex Proterozoic to Paleozoic history of the upper mantle recorded in the Urals lherzolite massifs by Re-Os and Sm-Nd systematics. Chemical Geology,2007,240:61-84
113.Batanova V G,Br(u|¨)gmann G E,Bazylev B A,et al.Platinum-group element abundances and Os isotope composition of mantle peridotites from the Mamonia complex,Cyprus.Chemical Geology,2008,248:195-212
114.Widom E,Kepezhinskas P,Defant M.The nature of metasomatism in the sub-arc mantle wedge:evidence from Re-Os isotopes in Kamchatka peridotite xenoliths.Chemical Geology,2003,196:283-306
115.Chesley J,Righter K,Ruiz J.Large-scale mantle metasomatism:a Re-Os perspective.Earth and Planetary Science Letters,2004,219:49-60
116.Gao S,Rudnick R L,Carlson R W,et al.Re-Os evidence for replacement of ancient mantle lithosphere beneath the North China craton.Earth and Planetary Science Letters,2002,198:307-322
117.Wu F Y,Walker R J,Yang Y H,et al.The chemical-temporal evolution of lithospheric mantle underlying the North China Craton.Geochimica et Cosmochimica Acta,2006,70:5013-5034
118.Yuan H L,Gao S,Rudnick R L,et al.Re-Os evidence for the age and origin of peridotites from the Dabie-Sulu ultrahigh pressure metamorphic belt,China.Chemical Geology,2007,236:323-338
119.Xu X S,Griffin W L,O'Reilly S Y,et al.Re-Os isotopes in sulfides of mantle peridotites from SE China:Age constraints and evolution of lithospheric mantle.Geochimica et Cosmochimica Acta,2003,(18s):A542
120.Xu X S,Griffin W L,O'Reilly S Y,et al.Re-Os isotopes of sulfides in mantle xenoliths from eastern China:progressive modification of lithospheric mantle.Lithos,2008,102:43-64
121.Xu Y G,Blusztajn J,Ma J L,et al.Late Archean to Early Proterozoic lithospheric mantle beneath the western North China craton:Sr-Nd-Os isotopes of peridotite xenoliths form Yangyuan and Fansi.Lithos,2008,102:25-42
122.Zhang H F,Goldstein S L,Zhou X H,et al.Evolution of subcontinental lithospheric mantle beneath eastern China:Re-Os isotopic evidence from mantle xenoliths in Paleozoic kimberlites and Mesozoic basalts.Contribution to Mineralogy and Petrology,2008,155:271-293
123．支霞臣，彭子成，陈道公，等．苏皖地区幔源橄榄岩捕虏体的锇同位素组成、模式年龄及其意义．岩石学报，2001，17(1)：11-18
124．支霞臣，彭子成，陈道公，等．苏皖地区大陆岩石圈地幔的长时性-地幔橄榄岩捕虏体的锇同位素模式年龄．中国科学(D辑)，2001，31(6)：464-470
125．支霞臣，秦协．中国东部地幔橄榄岩捕虏体的Re-Os同位素地球化学：岩石圈地幔的形成年龄和减薄作用的制约．岩石学报，2004，20(5)；989-998
126．支霞臣，郑永飞，杜安道，等．苏皖地区新生代玄武岩和幔源橄榄岩包体的~(187)Os／~(186)Os比值．科学通报，1996,41(3)：245-247
127．孙卫东，彭子成，支霞臣，等．N-TIMS法测定盘石山橄榄岩包体的锇同位素组成．科学通报．1997，42(21)：2310-2313
128．高山，Rudnick R L，Carlson R W，et a1．华北克拉通岩石圈地幔置换作用和壳幔生长耦合 的Re-Os同位素证据．地学前缘，2003，10(3)：61-67
129．夏琼霞，支霞臣，孟庆，等．汉诺坝幔源橄榄岩包体的微量元素和Re-Os同位素地球化学：SCLM的性质和形成时代．岩石学报，2004，20(5)：1215-1224
130．余淳梅，郑建平，Griffin W L．汉诺坝橄榄岩捕掳体原位Re-Os同位素年龄与多发地幔事件．科学通报，2007,31(1)：93-100
131．靳永斌，支霞臣，孟庆，等．大别山北部饶拔寨超镁铁岩体的形成时代：Re-Os同位素法定年．科学通报，2003,48(24)；2560-2565
132.Alard O,Griffin W L,Lorand J P,et al.Non-chondritic distribution of the highly siderophile elements in mantle sulphides.Nature,2000,407:891-894
133.Alard O,Luguet A,Pearson N J,et al.In situ Os isotopes in abyssal peridotites bridge the isotopic gap between MORBs and their source mantle.Nature,2005,436:1005-1008
134.Alard O,Griffin W L,Pearson N J,et al.New insights into the Re-Os systematics of sub-continental lithospheric mantle from in situ analysis of sulphides.Earth and Planetary Science Letters,2002,203:651-663
135.Griffin W L,Spetisus Z V,Pearson N J,et al.In situ Re-Os analysis of sulfide inclusions in kimberlitic olivine:New constraints on depletion events in the Siberian lithospheric mantle.Geochemistry,Geophysics,Geosystems,2002,3:1069-1094
136.Griffin W L,Graham S,O'Reilly S Y,et al.Lithosphere evolution beneath the Kaapvaal Craton:Re-Os systematic of sulfides in mantle-derived peridotites.Chemical Geology,2004,208:89-118
137.Pearson N J,Alard O,Griffin W L,et al.In situ measurement of Re-Os isotopes in mantle sulfides by laser ablation multicollector-inductively coupled plasma mass spectronmetry:analytical methods and preliminary results.Geochimica et Cosmochimica Acta,2002,66 (6):1037-1050
138.Wang K L,O'Reilly S Y,Griffin W L,et al.Proterozoic mantle lithosphere beneath the extended margin of the south China Block:In situ Re-Os evidence.Geology,2003,31(8):709-712
139.Pearson D G,Irvinea G J,Ionovb D A,et al.Re-Os isotope systematics and platinum group element fractionation during mantle melt extraction:a study of massif and xenolith peridotite suites.Chemical Geology,2004,208:29-59
140.Walker R J,Brandon A D,Bird J M,et al.~(187)Os-~(186)Os systematics of Os-Ir-Ru alloy grains from southwestem Oregon.Earth and Planetary Science Letters,2005,230:211-226
141.Pearson D G,Nowell G M.Dating mantle differentiation:a comparison of the Lu-Hf,Re-Os and Sm-Nd isotope systems in the Beni Bousera peridotite massif and constraints on the Nd-Hf composition of the lithospheric mantle.Geophys Res,2003,05430,Abstracts 5
142.Wittig N,Baker J A,Downes H.Dating the mantle roots of young continental crust.Geology,2006,34:237-240
143.Choi S H,Mukasa S B,Zhou X H,et al.Mantle dynamics beneath East Asia constrained by Sr,Nd,Pb and Hf isotopic systematics of ultramafic xenoliths and their host basalts from Hannuoba,North China.Chemical Geology,2008,248:40-61
144．张宏福，郑建平．华北中生代玄武岩的地球化学特征与岩石成因：以辽宁阜新为例．科学通报，2003，48(6)：603-609
145．许文良，郑常青，王冬艳．辽西中生代粗面玄武岩中地幔和下地壳捕虏体的发现及其地质意义．地质论评，1999，45(增)：444-449
146．裴福萍，许文良，王清海，等．鲁西费县中生代玄武岩及幔源捕虏晶的矿物化学：对岩石圈地幔性质的制约．高校地质学报，2004，10(1)：88-97
147．闫峻，陈江峰，谢智，等．鲁东晚白垩世玄武岩中的幔源捕虏体：对中国东部岩石圈减薄时间制约的新证据．科学通报，2003，48(14)：1570-1574
148.Ying J F,Zhang H F,Noriko K,et al.Nature and evolution of Late Cretaceous lithospheric mantle beneath the eastern North China Craton:Constraints from petrology and geochemistry of peridotitic xenoliths from Jtinan,Shandong province,China.Earth and Planetary Science Letters,2006,244:622-638
149．黄福生，薛绥洲．邢邯侵入体中幔源超镁铁质岩包体的发现及其矿物地球化学特征．岩石学报，1990，4：40-45
150．许文良，林景仟．河北邢邯地区角闪闪长岩中地幔纯橄岩包体的发现与研究．地质学报，1991，1：33-41
151．陈立辉，周新华．鲁西中生代闪长岩中的深源超镁铁质岩捕虏体及其富硅交代特征．中国科学(D辑)，2003,33(8)：735-744
152．余淳梅，郑建平，Griffin w L．汉诺坝橄榄岩捕虏体的单斜辉石LAM-ICPMS分析及其岩石圈地幔演化意义．地球科学—中国地质大学学报，2006,31(1)：93-100
153.Zhao G C,Cawood P A,Wilde S A,et al.Metamorphism of basement rocks in the Central Zone of the North China Craton:implications for Paleoproterozoic tectonic evolution.Precambrian Research,2000,103:55-88
154．马杏垣，白瑾，索书田等．中国前寒武纪构造格架及研究方法．北京：地质出版社，1987
155．伍家善，耿元生，沈其韩等．华北陆台早前寒武纪重大地质事件．北京：地质出版社，1991
156．伍家善，耿元生，沈其韩等．中朝古大陆太古宙地质特征及构造演化．北京：地质出版社，1998
157．程裕淇主编．华北地台早前寒武纪地质研究论文集．北京：地质出版社，1998
158．孙大中，陆松年．华北地台的元古宙构造演化．见：《孙大中文集》编委会．前寒武研究及可持续发展探索—孙大中文集．北京：地质出版社，1999
159．孙大中，翟安民．古华北陆台早前寒武纪地壳演化的几个问题的讨论．见： 《孙大中文集》编委会．前寒武研究及可持续发展探索—孙大中文集．北京：地质出版社，1999
160．邓晋福，吴宗絮，莫宣学等，华北地台前寒武花岗岩类陆壳演化与克拉通形成。岩石学报，1999，15(2)：190-198
161.Wang H Z and Mo X X.An outline of the tectonic evolution of China.Episodes,1995,18(1-2):6-16
162．邓晋福，罗照华，苏尚国等编著，岩石成因、构造环境与成矿作用。北京：地质出版社，2004
163．袁学诚．秦岭岩石圈速度结构与蘑菇云构造模型．中国科学(D辑)，1996，26(3)：209-215
164.Ren J,Tamaki K,Li S.Late Mesozoic and Cenozoic rifting and its dynamic setting in eastern China and adjacent areas.Tectonophysics,2002,344:175-205
165.Zhao G C,Wilde S A,Cawood P A,et al.Thermal evolution of two textural types of mafic granulites in the North China Craton:evidence for both mantle plume and collisional tectonics.Geological Mmagazine,1999,136:223-240
166.Zhao G C,Wilde S A,Cawood P A,et al.Archean blocks and their boundaries in the North China Craton:lithological,geochemical,structural and P-T path constraints and tectonic evolution.Precambrian Research,2001,107:45-73
167．赵国春，孙敏．华北克拉通基底构造单元特征及早元古代拼合．中国科学(D辑)，2002，32(7)：538-549
168.Sun M,Armstrong R L,Lambert R S J.Petrochemistry and Sr,Pb and Nd isotopic geochemistry of Early Precambrian rocks,Wutaishan and Taihangshan areas,China.Precambrian Research,1992,56:1-31
169.Robinson P T,Zhou M F,Hu X F,et al.Geochemical constraints on the origin of the Hegenshan ophiolite,Inner Mongolia,China.Journal of Asian Earth Sciences,1999,17:423-442
170．林景迁，谭冬娟，迟效国，等．胶辽半岛中生代花岗岩．北京：科学出版社，1992，17-23，72-88
171．路孝平，吴福元，赵成弼，等．通化地区印支期花岗岩锆石U-Pb年龄及其与大别-苏鲁超高压带碰撞造山作用之间的关系．科学通报，2003，48(8)：843-849
172．许文良，王清海，杨德彬，等．蚌埠荆山“混合花岗岩”SHRIMP锆石U-Pb定年及其地质意义．中国科学(D辑)，2004，34(5)：423-428
173．许文良，王冬艳，刘晓春，等．徐淮地区早侏罗世侵入杂岩体中榴辉岩类包体的发现及其地质意义．科学通报，2002，47(8)：618-622
174．陈立辉．山东莱芜中生代高镁侵入岩及其超镁铁质岩捕掳体的成因研究．[博士学位论文]，北京：中国科学院地质与地球物理研究所,2001，9-12
175．刘若新，陈文寄，孙建中，等．中国新生代火山岩的K-Ar年代学与构造环境．见：刘若新主编．中国新生代火山岩年代学与地球化学．北京：地震出版社，1992，1-43
176．王方正．山东山旺玄武岩的岩石学与地球化学特征．矿物学岩石学论丛，武汉：武汉地质学院出版社，1986，43-65
177．支霞臣．山东蓬莱、临朐新生代碱性玄武岩的痕量元素和岩石成因．地质论评，1990,36(5)：385-393
178．许继峰，邱家骧．山东临朐山旺地区玄武岩浆的分离结晶．地球科学-中国地质大学学报，1991，16(4)：369-376
179．陈道公，彭子成．山东新生代火山岩的K-Ar年龄和Sr-Pb回位素特征．地球化学，1985,4：293-303
180．狄明信，李永祥，白光勇．山东昌乐地区火山岩的岩石化学特征．石油大学学报(自然科学版)，1995，19(2)：7-11
181．孙平，路凤香，王主正，等．河南鹤壁尚峪新生代上地幔流变特征及构造意义．地球科学-中国地质大学学报，1996,21(1)：45-52
182．鄂莫岚，赵大升主编．中国东部新生代玄武岩及深源包体．北京：科学出版社，1987
183．马开义．依据重磁特征线图分析郯庐断裂带的南北延伸．辽宁地质学报，1983，(2)：11-18
184．赵文峰．下辽河依兰-伊通大陆裂谷形成演化与地震活动．构造地质论丛，1984，(3)：202-212
185．万天丰，朱鸿，赵磊，等．郯庐断裂带的形成与演化：综述．现代地质，1996，10(2)：159-168
186．陈宣华，王小凤，张青，等．郯庐断裂带形成演化的年代学研究．长春科技大学学报，2000,30(3)：215-220
187．刘顺，沈忠民，司建涛．郯庐断裂带演化动力学-多力源多时期分段作用模式．成都理工大学学报(自然科学版),2006,33(5)：473-477
188．徐嘉炜，马国锋．郯庐断裂带研究的十年回顾．地质论评，1992，38(4)：316-324．
189.Yin A,Nie S Y.An indentation model for the north and south China collision and development of the Tan-Lu andHonam fault systems,eastern Asia.Tectonics,1993,12(4):801-813
190．汤加富．大别山及邻区地质构造特征与形成演化-地幔差速环流与陆内多期造山．北京：地质出版社,2003
191．冯家麟，谢漫泽，张红，等．汉诺坝玄武岩及其深源包体．河北地质学院院报，1982，1：45-63
192．邱家骧，李昌年，李增田，等．汉诺坝玄武岩的主要特征及其形成的T、P、f_(O2)条件岩石矿物学杂志，1986，3(5)：193-202
193.Song Y,Frey F A,Zhi X C.Isotopoic characteristics of Hannuoba basalts,eastern China:Implications for their petrogenesis and the composition of Subcontinental mantle.Chemical Geology,1990,85:35-52
194.Zhi X C,Song Y,Frey F A,et al.Geochemistry of Hannuoba basalts,eastern China:constraints on the origin of continental alkalic and tholeiitic basalt.Chemical Geology,1990,88:1-33
195．李绍柄，刘德林，张振江，等．汉诺坝玄武岩稀土元素成分特征．地球化学，1987，4：351-359
196．谢广轰，王俊文，Tatsumoto M，等．汉诺坝玄武岩及大同火山群的岩石学和同位素地球化学．地球化学，1989,4：277-285
197．李天福，马鸿文．中国东部几个地区新生代玄武岩中单斜辉石-熔体平衡温压-兼论幔源包体的成因．岩石矿物学杂志，2002,21(1)：11-22
198．樊祺诚，刘若新．上地幔尖晶石—石榴石复合橄榄岩与相转变研究，中国矿物岩石地球化学学会地幔矿物岩石地球化学学会编，中国上地幔特征与动力学论文集，北京：地震出版社，1990：72-82
199．朱铭，胡华光，赵东植，等．山东省山旺地区新生代火山岩K-Ar年代学研究．岩石学研究，5：47-59
200．金隆裕．郑庐断裂带中段新生代玄武质岩石中的深源包体．长春地质学院学报，1985,3：21-32
201．郭正府，刘嘉麒，陈晓雨．山东山旺中新世火山喷发对生物生存环境的影响．中国科学，2007,37(9)：1169-1175
202.Norman M D,Pearson N J,Sharma A,et al.Quantitative analysis of trace elements in geological materials by laser ablation ICPMS:instrumental operating conditions and calibration values of NIST glasses.Geostand Newsl,1996,20,247-261.
203．路凤香和桑隆康主编．岩石学．北京：地质出版社，2002
204.Rivalenti G,Vannucci R,Rampone E,et al.Peridotite clinopyroxene chemistry reflects mantle processes rather than continental versus oceanic settings.Earth and Planetary Science Letters,139:423-437
205．陈绍海，周新华，张国辉，等．透辉石的激光探针ICP质谱分析及其深部地质意义．科学通报，1997,42(16)：1707-1711
206.Hauri E H,Hart S R.Constraints on the melt migration from mantle plumes:a trace element study of peridotite xenoliths from Savai'i,Western samoa.Journal of Geophysics Research,1994,99:24301-24322
207.Mitchell R H,Keays R R.Abundance and distribution of gold,palladium and iridium in some spinel and garnet lherzolites:implications for the nature and origin of precious metal-rich intergranular components in the upper mantle.Geochim Cosmochim Acta,1981,45:2425-2445
208.Roedder E.Fluid inclusion:Reviews in Mineralogy.Mineral.Soc.Am,1984,12:644
209.Anderson T,Griffin W L,O'Reilly S Y.Primary sulphide melt inclusions in mantle-derived megacrysts,Lithos,1987,20:279-294
210.Lorand J P.Sulfide petrology of spinel and gamet pyroenite layers from mantle-dirived spinel lherzolite massifs of Ariege,northeastern Pyrenees,France.J Petrol,1989,30:987-1015
211.Shaw C J S.Origin of sulfide blebs in variably metasomatized mantle xenoliths,quaterary West Eifel volcanic field,Gemany.Canadian Mineralogist,1997,35:1453-1463
212.Szabo C,Bodnar R J.Chemistry and origin of mantle sulfides in spinel peridotite xenoliths from alkaline basaltic lavas,Nograd-Gomor volcanic field,northern Hungary and southern Slovakia.Geochim.Cosmochim.Acta,1995,59:3917-3927
213．黄婉康，BasuA R．辉石巨晶中的硫化物及其成因．矿物学报．1987，7(2)：121-127
214．刘若新，樊祺诚，林卓然，等．地幔流体包裹体中多种固相充填物的发现及其意义．科学通报，1993,38(23)：2177-2180
215．徐九华，储雪蕾，邹一民，等．汉诺坝地幔捕虏体中的硫化物包裹体．科学通报，1998，43(13)：1438-1442．
216．徐九华，储雪蕾，谢玉玲，等．浙江新昌地幔岩捕虏体中的硫化物包裹体初步研究．地质论评，1999,4 5(6)：640-645
217．徐九华，谢玉玲，储雪蕾，等．中国东部地幔岩中的硫化物成分．矿床地质，2002,21(增)：1060-1063
218．储雪蕾，徐九华，赵善仁．地幔矿物中硫化物熔体包裹体的成因．地球物理学报，1998,4(增)：153-161
219.Guo J F,Griffin W L,O'Reilly S Y.Geochemistry and Origin of Sulphide Minerals in Mantle Xenoliths:Qilin,Southeastern China.Journal of Petrology,1999.40(7):1125-1149
220.Wells P R A.Pyroxene thermometry in simple and complex systems.Contrib.Mineral.Petrol,1977,62:129-139
221.Sachteben T,Seek H A.Chemical control of Al-solubility in orthopyroxene and its implications on pyroxene geochermometry.Contrib.Mineral.Petrol,1981,78:157-165
222. Brey, G, K(?)hler, T., 1990. Geochermobarometry in four-phase iherzolites.Ⅱ: New thermobarometers and practical assessment of existing thermobarometers. J.Petrol, 31, 1352-1378.
223. O'Reilly S Y, Griffin W L. 4-D lithosphere mapping: methodology and example. Tectonophysics, 1996, 262(1):3-18
224. McDonough W F, Sun S S. The composition of the Earth. Chem. Geol., 1995,120: 223-253
225. Claude T C. Lithosphere peridotites of the Kaapvaal Craton. Earth and Planetary Science Letters, 1993,120:13-29
226. Griffin W L, O'Reilly S Y and Ryan C G. The composition and origin of sub-continental lithospheric mantle. In Mantle Petrology: Field observations and high-pressure experimentation: A tribute to Francis R. (Joe) Boyd (eds. Fei Y, Berka C M and Mysen B O). The Geochemical Society, 1999(Special Publication), 6:13-45
227. Boyd F R. Origin of peridotite xenoliths: major element consideration. In high pressure and high temperature research on lithosphere and mantle materials (eds. Ranalli G, Ricci Lucchi F, Ricci C A, et al). University of Siena, Siena, 1996, 89-106
228. Boyd F R, Pearson D G, Nixon P H, et al. Low-calcium garnet harzburgites from southern Africa: their relations to craton structure and diamond crystallization. Contrib. Mineral. Petrol. 1993,113:352-366
229. Lee C T, Rudnick R L. Compositionally stratified cratonic lithosphere: petrology and geochemistry of peridotite xenoliths from the Labait volcano, Tanzania. In: Gurney J J, Gurney J L, Pascoe M D, et al(Eds.), The P H Nixon Volume. Proceedings Ⅶth International Kimberlite Conference. Red Roof Design, Cape Town, 1999,503-521
230. Sun S S, Mcdonough W F. Chemical and isotopic systematics of oceanic basalts: implications for mantle composition and processes. In: Saunders A D & Norry M J (eds). Magmatism in the Ocean Basins.Geological Society of London(Special Publication),42, 1989, 314-345
231. Johnson K T M, Dick H J B, Shimizu N. Melting in the oceanic upper mantle: An ion microprobe study of diopside in abyssal peridotites. J.Geophys.Res, 1990, 95: 2661-2678
232. Norman M D. Melting and metasomatism in the continental lithosphere: laser ablation ICPMS analysis of minerals in spinel lherzolites from eastern Australia. Contribution to Mineralogy and Petrology, 1998, 130,240-255
233. Wulff-Pedersen E, Neumann E R, Jensen B B. The upper mantle under La Palma, Canary Island: Formation of Si-K-Na-rich melt and its importance as a metasomatic agent. Comtrib.Mineral.Petrol, 1996,125: 113-139
234. Zangana N A, Downes H, Thirlwall M F, et al. Geochemical variation in peridotite xenoliths and their constituent clinopyroxenes from Ray Pic (?)French Massif Central.: implications for the composition of the shallow lithospheric mantle. Chem. Geol, 1999,153, 11-35
235. Meen J K. Mantle metasomatism and carbonates: an experimental study of a complex relationship. Geol. Soc. Am. (SpecPap), 1987,215:91-100
236. Yaxley G M, Green D H, Kamenetsky V. Carbonatite metasomatism in the southeastern Australia lithosphere.J Petrol,1998,39:1917-1930
237.Coltorti M,Bonadiman C,Hinton R W,et al.Carbonatite metasomatism of the oceanic upper mantle:evidence from clinopyroxenes and glasses in ultramafic xenoliths of Grande Comore,Indian Ocean.J.Petrol.,1999,40:133-165
238.Green D H.Experimental melting studies on a model upper mantle composition at high pressure under watersaturated and water-unsaturated conditions.Earth and Planetary Science Letters,1973 19,37-55
239.Green D H,Wallace M E.Mantle metasomatism by ephemeral carbonatite melts.Nature,1988,336,459-462
240．李天福，马鸿文，白志民．汉诺坝玄武岩的地球化学特征及成因模式．岩石矿物学杂志，1999， 18(3)：217-228
241.Palme H,O'Neill H St C.Cosmochemical estimates of mantle composition.In:Carlson R W(ed.).Treatise on Geochemistry:the mantle and core.Elsevier,2004,2:1-38
242.Bennett V C,Nutman A P,East T M.Constraints on mantle evolution from 187Os/188Os isotopic compositions of Archean ultramafic rocks from southern West Greenland (3.8Ga) and Western Australia (3.46Ga).Geochimica et Cosmochimica Acta,2002,66(14):2615-2630
243．支霞臣，Reisberg L，徐夕生．安徽女山幔源橄榄岩捕虏体Re-Os同位素地球化学．中国科学技术大学学报,2007,37(8)：945-952
244.Smoliar M I,Walker R J,Morgan J W.Re-Os ages of group ⅡA,ⅡA,IVB iron meteorites.Science,1996,271:1099-1102
245．徐义刚．岩石圈的热-机械侵蚀和化学侵蚀与岩石圈减薄．矿物岩石地球化学通报，1999，18(1)：1-5
246.Bird P.Initiation of intracontinental subduction in the Himalayas.Journal of Geophysics Research,1978,83(310):4975-4987
247．高山，金振民．拆沉作用(Delamination)及其壳-幔演化动力学意义．地质科技情报，1997，16(1)：1-9
248．高山，张本仁，金振民．秦岭-大别造山带下地壳拆沉作用．中国科学(D辑)，1999，29(6)：532-541
249．郑建平，孙敏，路凤香，等．信阳基性麻粒岩捕掳体及其华北南缘早中生代下地壳性质．岩石学报,2005,21(1)：91-98
250.Zhai M G,Fan Q C,Zhang H F,et al.Lower crustal processes leading to Mesozoic lithospheric thinning beneath eastern North China:underplating,replacement and delamination.Lithos,2007,96:36-54
251.Zheng J P,Griffin W L,O'Reilly S Y,et al.U-Pb and Hf-Isotope analysis of zircons in mafic xenoliths from Fuxian kimberlites:evolution of the lower crust beneath the North China Craton.Contribution to Mineralogy and Petrology,2004,148:79-103
252．侯贵廷，穆治国．华北克拉通晚前寒武纪镁铁质岩墙群K-Ar年龄及地质意义．华北地质矿产杂志，1994，9(3)：267-270
253．邵济安，张履桥，李大明．华北克拉通元古代的三次伸展事件．岩石学报,2002，18(2)：152-160
254．陆松年，李怀坤，李惠民，等．华北克拉通南缘龙王石童碱性花岗岩U-Pb年龄及其地质意义．地质通报，2003,22(12)：762-768
255．李宏基，李崇辉，杜利林．河北平山深熔伟晶岩锆石成因及SHRIPMP U-Pb年龄．自然科学进展，2004，14(17)：774-768
256.Zheng J P,Griffin W L,O'Reilly S Yet al.Zircons in mantle xenoliths record the Triassic Yangtze-North China continental collision.Earth Planetary Science Letters,2006,247:130-142
2.Zheng J P,Griffin W L,O'Reilly S Y,et al.3.6Ga lower crust in central China:new evidence on the assembly of the North China Craton.Geology,2004,32:229-232
3.Menzies M A,Fan W M & Zhang M.Paleozoic and Cenozoic lithoprobes and loss of＞120 km of Archaean lithosphere,Sino-Korean Craton,China.In:Prichard H M,Alabaster T,Harris N B W,et al (eds).Magmatic processes and plate tectonics.Geological Society of London,Special Publication no.76.1993,71-78
4.Menzies M A & Xu Y G.Geodynamics of the North China Craton.In:Flower M,Chung S L,Lo C H,et al (eds).Mantle dynamics and plate interactions in East Asia.American Geophysical Union Geodynamics Series no.27.Washington D C,1998,155-165
5.Griffin W L,Zhang A,O'Reilly S Y,et al.Phanerozoic evolution of the lithosphere beneath the Sino-Korean Craton.In:Flower M,Chung S L,Lo C H,et al (eds).Mantle dynamics and plate interactions in East Asia.American Geophysical Union Geodynamics Series no.27.Washington D C,1998,107-126
6.Xu Y G,Menzies M A,Mattey D P,et al.The nature of lithospheric mantle near the Tancheng-Lujiang fault,China:an integration of texture,chemistry and O-isotopes.Chemical Geology,1996,134:67-81
7.Fan W M,Zhang H F,Baker J,et al.On and off the North China Craton:where is the Archean keel? Journal of Petrology,2000,41:933-950
8． 郑建平．中国东部地幔置换作用与中新生代岩石圈减薄．武汉：中国地质大学出版社，1999
9． 邓晋福，赵海玲，莫宣学，等．中国大陆根柱构造-大陆动力学的钥匙．北京：地质出版社，1996，33-34
10．邓晋福，莫宣学，赵海玲，等．中国东部岩石圈根／去根作用与大陆“活化”-东亚型大陆动力学模式研究计划．现代地质，1994，8(3)：349-356
11．邓晋福，苏尚国，赵海玲，等．华北地区燕山期岩石圈减薄的深部过程．地学前缘,2003，10(3)：41-50
12．邓晋福，苏尚国，刘翠，等．关于华北克拉通燕山期岩石圈减薄的机制与过程的讨论：是拆沉，还是热侵蚀和化学交代?地学前缘，2006，13(2)：105-119
13．吴福元，孙德有．中国东部中生代岩浆作用与岩石圈减薄．长春科技大学学报，1999,29(4)：313-318
14．吴福元，葛文春，孙德有，等．中国东部岩石圈减薄研究中的几个问题．地学前缘,2003，10(3)：S1-60
15．吴福元，徐义刚，高山，等．华北岩石圈减薄与克拉通破坏研究的主要学术争论．岩石学报，2008，24(6)：1145-1174
16.Gao S,Rudnick R L,Yuan H L,et al.Recycling lower continental crust in the North China Craton.Nature,2004,432:892-897
17.Gao S,Rudnick R L,Xu W L,et al.Recycling deep cratonic lithosphere and generation of intraplate magmatism in the North China Craton.Earth and Planetary Science Letters,2008,270:41-53
18.Deng J F,Mo X X,Zhao H L,et al.2004.A new model for the dynamic evolution of Chinese lithosphere:‘continental roots-plume tectonics'.Earth-Science Reviews,2004,65:223-275
19.Deng J F,Su S G,Niu Y L,et al.A possible model for the lithospheric thinning of North China Craton:evidence form the Yanshanian (Jura-Cretaceous) magmatism and tectonism.Lithos,2007,96:22-35
20.Xu W L,Gao S,Wang Q H,et al.Mesozoic crustal thickening of the eastern North China craton:Evidence from eclogite xenoliths and petrologic implications.Geology,2006a,34(9):721-724
21.Xu W L,Wang Q H,Wang D Y,et al.Mesozoic adakitic rocks from the Xuzhou-Suzhou area,eastern China:Evidence for partial melting of delaminated lower continental crust.Journal of Asian Earth Sciences,2006b,27:454-464
22.Xu W L,Hergt J M,Gao S,et al.Interaction of adakitic melt-peridotite:implications for the high-Mg~# signature of Mesozoic adakitic rocks in the eastern North China Craton.Earth and Planetary Science Letters,2008,265:123-137
23.Xu Y G.Thermo-tectonic destruction of the Archean lithospheric keel beneath the Sino-Korean Craton in China:evidence,timing and mechanism.Physics and Chemistry of the Earth (A),2001,26(9-10):747-757
24.Xu Y G,Huang X L,Ma J L,et al.Crust-mantle interaction during the tectono-thermal reactivation of the North China Craton:constraints from SHRIMP zircon U-Pb chronology and geochemistry of Mesozoic plutons from western Shandong.Contribution to Mineralogy and Petrology,2004a,147:750-767
25.Zheng J P,O'Reilly S Y,Griffin W L,et al.Nature and evolution of Cenozoic lithospheric mantle beneath Shandong peninsula,Sino-Korean craton.International Geology Review,1998,40:471-499
26.Zheng J P,Griffin W L,O'Reilly S Y,et al.Late Mesozoic-Eocene mantle replacement beneath the eastern North China Craton:evidences from the Paleozoic and Cenozoic peridotite xenoliths.International Geology Review,2005,47:457-472
27.Zheng J P,Griffin,W L,O'Reilly,S Y,et al.Mineral chemistry of peridotites from Paleozoic,Mesozoic and Cenozoic lithosphere:constraints on mantle evolution beneath eastern China.Journal of Petrology,2006,47(11):2233-2256
28.Zheng J P,Griffin W L,O'Reilly S Y,et al.Mechanism and timing of lithospheric modification and replacement beneath the eastern North China Craton:Peridotitic xenoliths from the 100 Ma Fuxin basalts and a regional synthesis.Geochimica et Cosmochimica Acta,2007,71(21):5203-5225
29．张宏福，英基丰，徐平，等．华北中生代玄武岩中地幔橄榄石捕虏晶：对岩石圈地幔置换过程的启示．科学通报，2004，49(8)：784-789
30.Zhang H F,Sun M,Zhou X H,et al.Secular evolution of the lithosphere beneath the eastern North China Craton:Evidence from Mesozoic basalts and high-Mg andesites.Geochimica et Cosmochimica Acta,2003,67(22):4373-4387
31.Zhang H F,Ying J F,Shimoda G,et al.Importance of melt circulation and crust-mantle interaction in the lithospheric evolution beneath the North China Craton:evidence from Mesozoic basalts-borne clinopyroxene xenocrysts and pyroxenite xenoliths.Lithos,2007,96:67-89
32．姜耀辉，蒋少涌，赵葵东，等．辽东半岛煌斑岩SHRIMP锆石U-Pb年龄及其对中国东部岩石圈减薄开始时间的制约．科学通报,2005，50(19)：2161-2168
33．许文良，王冬艳，王清海，等．华北地块中东部中生代侵入杂岩中角闪石和黑云母的~(40)Ar/~(39)Ar定年：对岩石圈减薄时间的制约．地球化学，2004a,33(3)：221-231
34.Wu F Y,Walker R J,Ren X W,et al.Osmium isotopic constraints on the age of lithospheric mantle beneath Northeastern China.Chemical Geology,2003,196:107-129
35.Wu F Y,Lin J Q,Wilde S A,et al.Nature and significance of the Early Cretaceous giant igneous events in eastern China.Earth and Planetary Sciences Letters,2005,233:103-119
36.Zhang H F,Sun M,Zhou X H,et al.Geochemical constraints on the origin of Mesozoic alkaline intrusive complexes from the North China Craton and tectonic implications.Lithos,2005,81:297-317
37．伍家善，耿元生，沈其韩，等．华北陆台早前寒武纪重大地质事件．北京：地质出版社，1991
38．李继亮．五台山早元古代碰撞造山带的初步认识．地质科学，1990，1：1-11
39.Zhao G C,Wilde S A,Cawood P A,et al.Thermal evolution of Archean basement rocks from the eastern part of the Noryh Chian craton and its bearing on tectonic setting.International Geology Review,1998,40:706-721
40.Wang W.Formation of diamond with mineral inclusions of “mixed” eclogite and peridotite paragenesis.Earth and Planetary Science Letters,1998,160:831-843
41．路凤香，韩柱国，郑建平，等．辽宁复县地区古生代岩石圈地幔特征．地质科技情报，1991，10(增)：1-20
42．翟明国，朱日祥，刘建明，等．华北东部构造体制转折的关键时限．中国科学(D辑)，2003，33(10)：913-920
43．徐义刚．华北岩石圈减薄的时空不均一特征．高校地质学报，2004，10(3)：324-331
44．许文良，王清海，王冬艳，等．华北克拉通东部岩石圈减薄的过程与机制：中生代火成岩和深源捕虏体证据．地学前缘，2004b，11(3)：309-317
45．王晓蕊，高山，柳小明，等．辽西四合屯早白垩世义县组高镁安山岩的地球化学：对下地壳拆沉作用和Sr／Y变化的指示．中国科学(D辑)，2005，35(8)：700-709
46.Zhang H F,Sun M,Zhou X H,et al.Mesozoic lithosphere destruction beneath the North China Craton:evidence from major-,trace-element and Sr-Nd-Pb isotope studies of Fangcheng basalts.Contribution to Mineralogy and Petrology,2002,144:241-253
47.Fan W M,Guo F,Wang Y J,et al.Post-Orogenic bimodal volcanism along the Sulu orogenic belt in eastern China.Physics and Chemistry of the Earth (A),2001,26(9-10):733-746
48.Guo F,Fan W M,Wang Y J,et al.Origin of early Cretaceous calc-alkaline lamprophyres from the Sulu orogen in eastern China:implications for enrichment processes beneath continental collisional belt.Lithos,2004,78:291-305
49.Liu S,Hu R Z,Gao S,et al.U-Pb zircon age,geochemical and Sr-Nd-Pb-Hf isotopic constraints on age and origin of alkaline intrusions and associated mafic dikes from Sulu orogenic belt,Eastern China.Lithos,2008a,106:365-379
50.Tang H Y,Zheng J P,Yu C M.Age and composition of the Rushan intrusive complex in the northern Sulu orogen,eastern China:petrogenesis and lithospheric mantle evolution.Geological Magazine,2009,146(2):199-215
51.Xu Y G,Ma J L,Huang X L,et al.Early Cretaceous gabbroic complex from Yinan,Shandong Province:petrogenesis and mantle domains beneath the North China Craton.International Journal of Earth Science,2004b,93:1025-1041
52.Guo F,Fan W M,Wang Y J,et al.Late Mesozoic mafic intrusive complexes in North China Block:constraints on the nature of subcontinental lithospheric mantle.Physics and Chemistry of the Earth (A),2001,26(9-10):759-771
53.Ying J F,Zhou X H,Zhang H F.Geochemical and isotopic investigation of the Laiwu-Zibo carbonatites from western Shandong province,China and implications for their petrogenesis and enriched mantle source.Lithos,2004,75:413-426
54.Ying,J F,Zhou,X H,Zhang H E The geochemical variations of mid-Cretaceous lavas across western Shandong province,China and their tectonic implications.International Journal of Earth Science,2006a,95:68-79
55.Yang J H,Chung S L,Zhai M G,et al.Geochemical and Sr-Nd-Pb isotopic compositions of mafic dikes from the Jiaodong peninsula,China:evidence for vein-plus-peridotite melting in the lithospheric mantle.Lithos,2004,73:145-160
56.Liu S,Hu R Z,Gao S,et al.Zircon U-Pb geochronology and major,trace elemental and Sr-Nd-Pb isotopic geochemistry of mafic dykes in western Shandong Province,eastern China:Constraints on their petrogenesis and geodynamic significance.Chemical Geology,2008b,255:329-345
57．杨进辉，朱美妃，刘伟，等．胶东地区郭家岭花岗闪长岩的地球化学特征及成因．岩石学报，2003，19(4)：692-700
58．袁洪林，柳小明，刘勇胜，等．北京西山晚中生代火山岩U-Pb锆石年代学及地球化学研究．中国科学(D辑)，2005，35(9)：821-836
59．杨承海，许文良，杨德彬，等．鲁西中生代高Mg闪长岩的成因：年代学与岩石地球化学证据．地球科学-中国地质大学学报，2006，31(1)：81-92
60．杨承海，许文良，杨德彬，等．鲁西上峪辉长-闪长岩的成因：年代学与岩石地球化学证据．中国科学(D辑)，2008，38(1)：44-55
61.Chen B,Jahn B M,Arakawa Y,et al.Petrogenesis of the Mesozoic intrusive complexes from the southern Taihang orogen,North China Craton:elemental and Sr-Nd-Pb isotopic constraints.Contribution to Mineralogy and Petrology,2004,148:489-501
62.Chen B,Zhai M G.Geochemistry of late Mesozoic lamprophyre dykes from the Taihang Mountains,North China,and implications for the sub-continental lithospheric mantle.Geological Magazine,2003,140:87-93
63.Chen B,Tian W,Jahn B M,et al.Zircon SHRIMP U-Pb ages and in-situ Hf isotopic analysis for the Mesozoic intrusions in Southern Taihang,North China craton:evidence for hybridization between mantle-derived magmas and crustal components.Lithos,2008,102(1-2):118-137
64.Wang Y J,Fan W M,Zhang H F,et al.Early Cretaceous gabbroic rocks from the Taihang Mountains:implications for a paleosubduction-related lithospheric mantle beneath the central North China Craton.Lithos,2006,86:281-302
65．陈斌，田伟，翟明国，等．太行山和华北其它地区中生代岩浆作用的锆石U-Pb年代学和地球化学特征及其岩浆成因和地球动力学意义．岩石学报，2005，21(1)：13-24
66．陈斌，翟明国，邵济安．太行山北段中生代岩基的成因和意义：主要和微量元素地球化学证据．中国科学(D辑)，2002,32(11)：896-907
67．蔡剑辉，阎国翰，肖成东，等．太行山大兴安岭构造岩浆带中生代侵入岩Nd、sr、Pb同位素特征及物质来源探讨．岩石学报，2004，20(5)：1225-1242
68．彭头平，王岳军，范蔚茗，等．南太行山闪长岩的SHRIMP锆石U-Pb年龄及岩石成因研究．岩石学报，2004，20(5)：1253-1262
69．许文良，王冬艳，高山，等．鲁西中生代金岭闪长岩中纯橄岩和辉石岩包体的发现及其意义．科学通报，2003a，48(8)：863-868
70．许文良，王冬艳，王清海，等．鲁西中生代闪长岩中两类幔源捕虏体的岩石学和地球化学．岩石学报,2003b，19(4)：623-636
71.Zheng J P,Sun M,Zhou M F,et al.Trace elemental and PGE geochemical constraints of Mesozoic and Cenozoic peridotitic xenoliths on lithospheric evolution of the North China Craton.Geochimica et Cosmochimica Acta,2005,69(13):3401-3418
72.Zhang H F,Sun M,Zhou M F,et al.Highly heterogeneous late Mesozoic lithospheric mantle beneath the North China Craton:evidence from Sr-Nd-Pb isotopic systematics of mafic igneous rocks.Geological Magazine,2004,141:55-62
73．张儒媛，从柏林．安徽女山碧玄岩及其榄岩类包体的成因岩石学和大地构造意义．岩石学研究，1983，(3)：111-128
74.Xu X S,O'Reilly S Y,Griffin W L,et al.The nature of the Cenozoic lithosphere beneath Nushan,East Central China.Flower M F J,Chung S L,Lo C H,et al.Mantle Dynamics and Plate Interactions in East Asia.American Geophysical Union,1998,117-138
75.Song Y,Frey F A.Geochemistry of peridotite xenoliths in basalt from Hannuoba,Eastern China:Implications for Subcontinental mantle heterogeneity.Geochimica et Cosmochimica Acta,1989,53:97-113
76.Chen,S H,O'Reilly,S Y,Zhou X H,et al.Thermal and petrological structure of the lithosphere beneath Hannuoba,Sino-Korean Craton,China:evidence from xenoliths.Lithos, 2001,56:267-301
77.Rudnick R L,Gao S,Ling W L,et al.Petrology and geochemistry of spinel peridotite xenoliths from Hannuoba and Qixia,North China craton.Lithos,2004,77:609-637
78．鄂莫岚，路凤香，邓晋福．吉林汪清超镁铁岩包体的岩石学特征及辉石岩成因问题的讨论．地球化学，1982，18：39-56
79．方同辉，马鸿文．辽宁宽甸地区上地幔岩石圈组成及热结构．地质论评，1999，45(增)：450-457
80．路凤香，郑建平．华北地台古生代岩石圈地幔特征及深部过程．见：池际尚，路凤香主编，华北地台金伯利岩及古生代岩石圈地幔特征，北京：科学出版社，1996
81.Zheng J P,O'Reilly S Y,Griffin W L,et al.Relict refractory mantle beneath the eastern North China block:significance for lithosphere evolution.Lithos,2001:57:43-66
82.Gao S,Zhang B R,Jin Z M,et al.How mafic is the lower continental crust? Earth planetary Science Letter,1998,161:101-117
83．路凤香，郑建平，李伍平，等．中国东部显生宙地幔演化的主要样式：“蘑菇云”模型．地学前缘，2000,7(1)：97-107
84．路凤香，郑建平，邵济安，等．华北东部中生代晚期-新生代软流圈上涌与岩石圈减薄．地学前缘,2006，13(2)：86-92
85.Zhang H F.Transformation of lithospheric mantle through peridotite-melt reaction:a case of Sino-Korean craton.Earth and Planetary Science Letters,2005,237:768-780
86．张宏福，周新华，范蔚茗，等．华北东南部中生代岩石圈地幔性质、组成、富集过程及其形成机理．岩石学报，2005，21(4)：1271-1280
87．支霞臣．Re-Os同位素体系和大陆岩石圈地幔定年．科学通报，1999,44(22)：2362-2371
88.Walker R J,Carlson R W,Shirey S B,et al.Os,Sr,Nd and Pb isotope systematics of southern African peridotite xenoliths:implications for the chemical evolution of Subcontinental mantle.Geochimica et Cosmochimica Acta,1989,53:3005-3013
89.Carlson R W,Irving A J.Depletion and enrichment history of subcontinental lithospheric mantle an Os,Sr,Nd and Pb isotopic study of ultramafic xenoliths from the northwestern Wyoming Craton.Earth and Planetary Science Letters,1994,126:457-472
90.Pearson D G,Carlson R W,Shirey S B,et al.The stabilization of Archaean lithospheric mantle:a Re-Os isotope study of peridotite xenoliths from the Kaapvaal and Siberian cratons.Earth and Planetary Science Letters,1995,134:341-357
91.Pearson D G.The age of continental roots.Lithos,1999,48:171-194
92.Shirey S B,Walker R J.The Re-Os isotope system in cosmochemistry and high-temperature geochemistry.Annu.Rev.Earth Planet.Sci.,1998,26:423-500
93.Meisel T,Walker R J,Irving A J,et al.Osmium isotopic compositions of mantle xenoliths:A global perspective.Geochimica et Cosmochimica Acta,2001,65(8):1311-1323
94.Carlson R W.Application of the Pt-Re-Os isotopic systems to mantle geochemistry and geochronology.Lithos,2005,82:249-272
95.Faure G.Principles of Isotope Geology,John Wiley & sons,Inc.,1986,264-268
96.Reisberg L,Lorand J P.Longevity of sub-continental mantle lithosphere from osmium isotope systematics in orogenic peridotite massifs.Nature,1995,376:159-162
97．吴福元，杨进辉，储著银，等．大陆岩石圈地幔定年．地学前缘，2007，14(2)：76-86
98.Schmitz M D,Bowring S A,Wit M J.Subduction and terrane collision stabilize the western Kaapvaal craton tectosphere 2.9 billion years ago.Earth and Planetary Science Letters,2004,222:363-376
99.Irvine G J,Pearson D G,Kjarsgaard B A.A Re-Os isotope and PGE study of kimberlite-derived peridotite xenoliths from Somerset Island and a comparison to the Slave and Kaapvaal cratons.Lithos,2003,71:46t-488
100.Olive V,Ellam R M,Harte B.A Re-Os isotope study of ultramafic xenoliths from the Matsoku kimberlite.Earth and Planetary Science Letters,1997,150:129-140
101.Pearson D G,Snyder G A,Shirey S B,et al.Archean Re-Os age for Siberian eclogites and constrains on Archean tectonics.Nature,1995,374:711-713
102.Peslier A H,Reisberg L,Ludden J,et al.Os isotopic systematics in mantle xenoliths;age constraints on the Canadian Cordillera lithosphere.Chemical Geology,2000,166:85-101
103.Handler M R,Wysoczanski R J,Gamble J A.Proterozoic lithosphere in Marie Byrd Land,West Antarctica:Re-Os systematics of spinel peridotite xenoliths.Chemical Geology,2003,196:131-145
104.Lee S R,Walker R J.Re-Os isotope systematics of mantle xenoliths from South Korea:evidence for complex growth and loss of lithospheric mantle beneath East Asia.Chemical Geology,2006,231:90-101
105.Schilling M E,Carlson R W,Conceic~o R V.Re-Os isotope constraints on subcontinental lithospheric mantle evolution of southern South America.Earth and Planetary Science Letters,2008,268:89-101
106.Burnham O M,Rogers N W,Pearson D G,et al.The petrogenesis of the eastern Pyrenean peridotites:An integrated study of their whole-rock geochemistry and Re-Os isotope composition.Geochimica et Cosmochimica Acta,1998,62(13):2293-2310
107.Reisberg L,Allegre C J,Luck J M.The Re-Os systematics of Ronda ultramafic complex of southern Spain.Earth and Planetary Science Letters,1991,105:196-219
108.Roy-Barman M,Allegre C J.~(187)Os/~(186)Os ratios of mid-ocean ridge basalts and abyssal peridotites.Geochimica et Cosmochimica Acta,1994,(58):5043-5054
109.Meisel T,Walker R J,Morgen J W.The osmium isotopic composition of the Earth's primitive upper mantle.Nature,1996,383:517-520
110.Meisel T,Melcher F,Tomascak P,et al.Re-Os isotopes in orogenic peridotite massifs in the Eastern Alps,Austria.Chemical Geology,1997,143:217-229
111.Harvey J,Garmoun A,Burton K W,et al.Ancient melt extraction from the oceanic upper mantle revealed by Re-Os isotopes in abyssal peridotites from the Mid-Atlantic ridge.Earth and Planetary Science Letters,2006,244:606-621
112.Tessalina S G,Bourdon B,Gannoun A,et al.Complex Proterozoic to Paleozoic history of the upper mantle recorded in the Urals lherzolite massifs by Re-Os and Sm-Nd systematics. Chemical Geology,2007,240:61-84
113.Batanova V G,Br(u|¨)gmann G E,Bazylev B A,et al.Platinum-group element abundances and Os isotope composition of mantle peridotites from the Mamonia complex,Cyprus.Chemical Geology,2008,248:195-212
114.Widom E,Kepezhinskas P,Defant M.The nature of metasomatism in the sub-arc mantle wedge:evidence from Re-Os isotopes in Kamchatka peridotite xenoliths.Chemical Geology,2003,196:283-306
115.Chesley J,Righter K,Ruiz J.Large-scale mantle metasomatism:a Re-Os perspective.Earth and Planetary Science Letters,2004,219:49-60
116.Gao S,Rudnick R L,Carlson R W,et al.Re-Os evidence for replacement of ancient mantle lithosphere beneath the North China craton.Earth and Planetary Science Letters,2002,198:307-322
117.Wu F Y,Walker R J,Yang Y H,et al.The chemical-temporal evolution of lithospheric mantle underlying the North China Craton.Geochimica et Cosmochimica Acta,2006,70:5013-5034
118.Yuan H L,Gao S,Rudnick R L,et al.Re-Os evidence for the age and origin of peridotites from the Dabie-Sulu ultrahigh pressure metamorphic belt,China.Chemical Geology,2007,236:323-338
119.Xu X S,Griffin W L,O'Reilly S Y,et al.Re-Os isotopes in sulfides of mantle peridotites from SE China:Age constraints and evolution of lithospheric mantle.Geochimica et Cosmochimica Acta,2003,(18s):A542
120.Xu X S,Griffin W L,O'Reilly S Y,et al.Re-Os isotopes of sulfides in mantle xenoliths from eastern China:progressive modification of lithospheric mantle.Lithos,2008,102:43-64
121.Xu Y G,Blusztajn J,Ma J L,et al.Late Archean to Early Proterozoic lithospheric mantle beneath the western North China craton:Sr-Nd-Os isotopes of peridotite xenoliths form Yangyuan and Fansi.Lithos,2008,102:25-42
122.Zhang H F,Goldstein S L,Zhou X H,et al.Evolution of subcontinental lithospheric mantle beneath eastern China:Re-Os isotopic evidence from mantle xenoliths in Paleozoic kimberlites and Mesozoic basalts.Contribution to Mineralogy and Petrology,2008,155:271-293
123．支霞臣，彭子成，陈道公，等．苏皖地区幔源橄榄岩捕虏体的锇同位素组成、模式年龄及其意义．岩石学报，2001，17(1)：11-18
124．支霞臣，彭子成，陈道公，等．苏皖地区大陆岩石圈地幔的长时性-地幔橄榄岩捕虏体的锇同位素模式年龄．中国科学(D辑)，2001，31(6)：464-470
125．支霞臣，秦协．中国东部地幔橄榄岩捕虏体的Re-Os同位素地球化学：岩石圈地幔的形成年龄和减薄作用的制约．岩石学报，2004，20(5)；989-998
126．支霞臣，郑永飞，杜安道，等．苏皖地区新生代玄武岩和幔源橄榄岩包体的~(187)Os／~(186)Os比值．科学通报，1996,41(3)：245-247
127．孙卫东，彭子成，支霞臣，等．N-TIMS法测定盘石山橄榄岩包体的锇同位素组成．科学通报．1997，42(21)：2310-2313
128．高山，Rudnick R L，Carlson R W，et a1．华北克拉通岩石圈地幔置换作用和壳幔生长耦合 的Re-Os同位素证据．地学前缘，2003，10(3)：61-67
129．夏琼霞，支霞臣，孟庆，等．汉诺坝幔源橄榄岩包体的微量元素和Re-Os同位素地球化学：SCLM的性质和形成时代．岩石学报，2004，20(5)：1215-1224
130．余淳梅，郑建平，Griffin W L．汉诺坝橄榄岩捕掳体原位Re-Os同位素年龄与多发地幔事件．科学通报，2007,31(1)：93-100
131．靳永斌，支霞臣，孟庆，等．大别山北部饶拔寨超镁铁岩体的形成时代：Re-Os同位素法定年．科学通报，2003,48(24)；2560-2565
132.Alard O,Griffin W L,Lorand J P,et al.Non-chondritic distribution of the highly siderophile elements in mantle sulphides.Nature,2000,407:891-894
133.Alard O,Luguet A,Pearson N J,et al.In situ Os isotopes in abyssal peridotites bridge the isotopic gap between MORBs and their source mantle.Nature,2005,436:1005-1008
134.Alard O,Griffin W L,Pearson N J,et al.New insights into the Re-Os systematics of sub-continental lithospheric mantle from in situ analysis of sulphides.Earth and Planetary Science Letters,2002,203:651-663
135.Griffin W L,Spetisus Z V,Pearson N J,et al.In situ Re-Os analysis of sulfide inclusions in kimberlitic olivine:New constraints on depletion events in the Siberian lithospheric mantle.Geochemistry,Geophysics,Geosystems,2002,3:1069-1094
136.Griffin W L,Graham S,O'Reilly S Y,et al.Lithosphere evolution beneath the Kaapvaal Craton:Re-Os systematic of sulfides in mantle-derived peridotites.Chemical Geology,2004,208:89-118
137.Pearson N J,Alard O,Griffin W L,et al.In situ measurement of Re-Os isotopes in mantle sulfides by laser ablation multicollector-inductively coupled plasma mass spectronmetry:analytical methods and preliminary results.Geochimica et Cosmochimica Acta,2002,66 (6):1037-1050
138.Wang K L,O'Reilly S Y,Griffin W L,et al.Proterozoic mantle lithosphere beneath the extended margin of the south China Block:In situ Re-Os evidence.Geology,2003,31(8):709-712
139.Pearson D G,Irvinea G J,Ionovb D A,et al.Re-Os isotope systematics and platinum group element fractionation during mantle melt extraction:a study of massif and xenolith peridotite suites.Chemical Geology,2004,208:29-59
140.Walker R J,Brandon A D,Bird J M,et al.~(187)Os-~(186)Os systematics of Os-Ir-Ru alloy grains from southwestem Oregon.Earth and Planetary Science Letters,2005,230:211-226
141.Pearson D G,Nowell G M.Dating mantle differentiation:a comparison of the Lu-Hf,Re-Os and Sm-Nd isotope systems in the Beni Bousera peridotite massif and constraints on the Nd-Hf composition of the lithospheric mantle.Geophys Res,2003,05430,Abstracts 5
142.Wittig N,Baker J A,Downes H.Dating the mantle roots of young continental crust.Geology,2006,34:237-240
143.Choi S H,Mukasa S B,Zhou X H,et al.Mantle dynamics beneath East Asia constrained by Sr,Nd,Pb and Hf isotopic systematics of ultramafic xenoliths and their host basalts from Hannuoba,North China.Chemical Geology,2008,248:40-61
144．张宏福，郑建平．华北中生代玄武岩的地球化学特征与岩石成因：以辽宁阜新为例．科学通报，2003，48(6)：603-609
145．许文良，郑常青，王冬艳．辽西中生代粗面玄武岩中地幔和下地壳捕虏体的发现及其地质意义．地质论评，1999，45(增)：444-449
146．裴福萍，许文良，王清海，等．鲁西费县中生代玄武岩及幔源捕虏晶的矿物化学：对岩石圈地幔性质的制约．高校地质学报，2004，10(1)：88-97
147．闫峻，陈江峰，谢智，等．鲁东晚白垩世玄武岩中的幔源捕虏体：对中国东部岩石圈减薄时间制约的新证据．科学通报，2003，48(14)：1570-1574
148.Ying J F,Zhang H F,Noriko K,et al.Nature and evolution of Late Cretaceous lithospheric mantle beneath the eastern North China Craton:Constraints from petrology and geochemistry of peridotitic xenoliths from Jtinan,Shandong province,China.Earth and Planetary Science Letters,2006,244:622-638
149．黄福生，薛绥洲．邢邯侵入体中幔源超镁铁质岩包体的发现及其矿物地球化学特征．岩石学报，1990，4：40-45
150．许文良，林景仟．河北邢邯地区角闪闪长岩中地幔纯橄岩包体的发现与研究．地质学报，1991，1：33-41
151．陈立辉，周新华．鲁西中生代闪长岩中的深源超镁铁质岩捕虏体及其富硅交代特征．中国科学(D辑)，2003,33(8)：735-744
152．余淳梅，郑建平，Griffin w L．汉诺坝橄榄岩捕虏体的单斜辉石LAM-ICPMS分析及其岩石圈地幔演化意义．地球科学—中国地质大学学报，2006,31(1)：93-100
153.Zhao G C,Cawood P A,Wilde S A,et al.Metamorphism of basement rocks in the Central Zone of the North China Craton:implications for Paleoproterozoic tectonic evolution.Precambrian Research,2000,103:55-88
154．马杏垣，白瑾，索书田等．中国前寒武纪构造格架及研究方法．北京：地质出版社，1987
155．伍家善，耿元生，沈其韩等．华北陆台早前寒武纪重大地质事件．北京：地质出版社，1991
156．伍家善，耿元生，沈其韩等．中朝古大陆太古宙地质特征及构造演化．北京：地质出版社，1998
157．程裕淇主编．华北地台早前寒武纪地质研究论文集．北京：地质出版社，1998
158．孙大中，陆松年．华北地台的元古宙构造演化．见：《孙大中文集》编委会．前寒武研究及可持续发展探索—孙大中文集．北京：地质出版社，1999
159．孙大中，翟安民．古华北陆台早前寒武纪地壳演化的几个问题的讨论．见： 《孙大中文集》编委会．前寒武研究及可持续发展探索—孙大中文集．北京：地质出版社，1999
160．邓晋福，吴宗絮，莫宣学等，华北地台前寒武花岗岩类陆壳演化与克拉通形成。岩石学报，1999，15(2)：190-198
161.Wang H Z and Mo X X.An outline of the tectonic evolution of China.Episodes,1995,18(1-2):6-16
162．邓晋福，罗照华，苏尚国等编著，岩石成因、构造环境与成矿作用。北京：地质出版社，2004
163．袁学诚．秦岭岩石圈速度结构与蘑菇云构造模型．中国科学(D辑)，1996，26(3)：209-215
164.Ren J,Tamaki K,Li S.Late Mesozoic and Cenozoic rifting and its dynamic setting in eastern China and adjacent areas.Tectonophysics,2002,344:175-205
165.Zhao G C,Wilde S A,Cawood P A,et al.Thermal evolution of two textural types of mafic granulites in the North China Craton:evidence for both mantle plume and collisional tectonics.Geological Mmagazine,1999,136:223-240
166.Zhao G C,Wilde S A,Cawood P A,et al.Archean blocks and their boundaries in the North China Craton:lithological,geochemical,structural and P-T path constraints and tectonic evolution.Precambrian Research,2001,107:45-73
167．赵国春，孙敏．华北克拉通基底构造单元特征及早元古代拼合．中国科学(D辑)，2002，32(7)：538-549
168.Sun M,Armstrong R L,Lambert R S J.Petrochemistry and Sr,Pb and Nd isotopic geochemistry of Early Precambrian rocks,Wutaishan and Taihangshan areas,China.Precambrian Research,1992,56:1-31
169.Robinson P T,Zhou M F,Hu X F,et al.Geochemical constraints on the origin of the Hegenshan ophiolite,Inner Mongolia,China.Journal of Asian Earth Sciences,1999,17:423-442
170．林景迁，谭冬娟，迟效国，等．胶辽半岛中生代花岗岩．北京：科学出版社，1992，17-23，72-88
171．路孝平，吴福元，赵成弼，等．通化地区印支期花岗岩锆石U-Pb年龄及其与大别-苏鲁超高压带碰撞造山作用之间的关系．科学通报，2003，48(8)：843-849
172．许文良，王清海，杨德彬，等．蚌埠荆山“混合花岗岩”SHRIMP锆石U-Pb定年及其地质意义．中国科学(D辑)，2004，34(5)：423-428
173．许文良，王冬艳，刘晓春，等．徐淮地区早侏罗世侵入杂岩体中榴辉岩类包体的发现及其地质意义．科学通报，2002，47(8)：618-622
174．陈立辉．山东莱芜中生代高镁侵入岩及其超镁铁质岩捕掳体的成因研究．[博士学位论文]，北京：中国科学院地质与地球物理研究所,2001，9-12
175．刘若新，陈文寄，孙建中，等．中国新生代火山岩的K-Ar年代学与构造环境．见：刘若新主编．中国新生代火山岩年代学与地球化学．北京：地震出版社，1992，1-43
176．王方正．山东山旺玄武岩的岩石学与地球化学特征．矿物学岩石学论丛，武汉：武汉地质学院出版社，1986，43-65
177．支霞臣．山东蓬莱、临朐新生代碱性玄武岩的痕量元素和岩石成因．地质论评，1990,36(5)：385-393
178．许继峰，邱家骧．山东临朐山旺地区玄武岩浆的分离结晶．地球科学-中国地质大学学报，1991，16(4)：369-376
179．陈道公，彭子成．山东新生代火山岩的K-Ar年龄和Sr-Pb回位素特征．地球化学，1985,4：293-303
180．狄明信，李永祥，白光勇．山东昌乐地区火山岩的岩石化学特征．石油大学学报(自然科学版)，1995，19(2)：7-11
181．孙平，路凤香，王主正，等．河南鹤壁尚峪新生代上地幔流变特征及构造意义．地球科学-中国地质大学学报，1996,21(1)：45-52
182．鄂莫岚，赵大升主编．中国东部新生代玄武岩及深源包体．北京：科学出版社，1987
183．马开义．依据重磁特征线图分析郯庐断裂带的南北延伸．辽宁地质学报，1983，(2)：11-18
184．赵文峰．下辽河依兰-伊通大陆裂谷形成演化与地震活动．构造地质论丛，1984，(3)：202-212
185．万天丰，朱鸿，赵磊，等．郯庐断裂带的形成与演化：综述．现代地质，1996，10(2)：159-168
186．陈宣华，王小凤，张青，等．郯庐断裂带形成演化的年代学研究．长春科技大学学报，2000,30(3)：215-220
187．刘顺，沈忠民，司建涛．郯庐断裂带演化动力学-多力源多时期分段作用模式．成都理工大学学报(自然科学版),2006,33(5)：473-477
188．徐嘉炜，马国锋．郯庐断裂带研究的十年回顾．地质论评，1992，38(4)：316-324．
189.Yin A,Nie S Y.An indentation model for the north and south China collision and development of the Tan-Lu andHonam fault systems,eastern Asia.Tectonics,1993,12(4):801-813
190．汤加富．大别山及邻区地质构造特征与形成演化-地幔差速环流与陆内多期造山．北京：地质出版社,2003
191．冯家麟，谢漫泽，张红，等．汉诺坝玄武岩及其深源包体．河北地质学院院报，1982，1：45-63
192．邱家骧，李昌年，李增田，等．汉诺坝玄武岩的主要特征及其形成的T、P、f_(O2)条件岩石矿物学杂志，1986，3(5)：193-202
193.Song Y,Frey F A,Zhi X C.Isotopoic characteristics of Hannuoba basalts,eastern China:Implications for their petrogenesis and the composition of Subcontinental mantle.Chemical Geology,1990,85:35-52
194.Zhi X C,Song Y,Frey F A,et al.Geochemistry of Hannuoba basalts,eastern China:constraints on the origin of continental alkalic and tholeiitic basalt.Chemical Geology,1990,88:1-33
195．李绍柄，刘德林，张振江，等．汉诺坝玄武岩稀土元素成分特征．地球化学，1987，4：351-359
196．谢广轰，王俊文，Tatsumoto M，等．汉诺坝玄武岩及大同火山群的岩石学和同位素地球化学．地球化学，1989,4：277-285
197．李天福，马鸿文．中国东部几个地区新生代玄武岩中单斜辉石-熔体平衡温压-兼论幔源包体的成因．岩石矿物学杂志，2002,21(1)：11-22
198．樊祺诚，刘若新．上地幔尖晶石—石榴石复合橄榄岩与相转变研究，中国矿物岩石地球化学学会地幔矿物岩石地球化学学会编，中国上地幔特征与动力学论文集，北京：地震出版社，1990：72-82
199．朱铭，胡华光，赵东植，等．山东省山旺地区新生代火山岩K-Ar年代学研究．岩石学研究，5：47-59
200．金隆裕．郑庐断裂带中段新生代玄武质岩石中的深源包体．长春地质学院学报，1985,3：21-32
201．郭正府，刘嘉麒，陈晓雨．山东山旺中新世火山喷发对生物生存环境的影响．中国科学，2007,37(9)：1169-1175
202.Norman M D,Pearson N J,Sharma A,et al.Quantitative analysis of trace elements in geological materials by laser ablation ICPMS:instrumental operating conditions and calibration values of NIST glasses.Geostand Newsl,1996,20,247-261.
203．路凤香和桑隆康主编．岩石学．北京：地质出版社，2002
204.Rivalenti G,Vannucci R,Rampone E,et al.Peridotite clinopyroxene chemistry reflects mantle processes rather than continental versus oceanic settings.Earth and Planetary Science Letters,139:423-437
205．陈绍海，周新华，张国辉，等．透辉石的激光探针ICP质谱分析及其深部地质意义．科学通报，1997,42(16)：1707-1711
206.Hauri E H,Hart S R.Constraints on the melt migration from mantle plumes:a trace element study of peridotite xenoliths from Savai'i,Western samoa.Journal of Geophysics Research,1994,99:24301-24322
207.Mitchell R H,Keays R R.Abundance and distribution of gold,palladium and iridium in some spinel and garnet lherzolites:implications for the nature and origin of precious metal-rich intergranular components in the upper mantle.Geochim Cosmochim Acta,1981,45:2425-2445
208.Roedder E.Fluid inclusion:Reviews in Mineralogy.Mineral.Soc.Am,1984,12:644
209.Anderson T,Griffin W L,O'Reilly S Y.Primary sulphide melt inclusions in mantle-derived megacrysts,Lithos,1987,20:279-294
210.Lorand J P.Sulfide petrology of spinel and gamet pyroenite layers from mantle-dirived spinel lherzolite massifs of Ariege,northeastern Pyrenees,France.J Petrol,1989,30:987-1015
211.Shaw C J S.Origin of sulfide blebs in variably metasomatized mantle xenoliths,quaterary West Eifel volcanic field,Gemany.Canadian Mineralogist,1997,35:1453-1463
212.Szabo C,Bodnar R J.Chemistry and origin of mantle sulfides in spinel peridotite xenoliths from alkaline basaltic lavas,Nograd-Gomor volcanic field,northern Hungary and southern Slovakia.Geochim.Cosmochim.Acta,1995,59:3917-3927
213．黄婉康，BasuA R．辉石巨晶中的硫化物及其成因．矿物学报．1987，7(2)：121-127
214．刘若新，樊祺诚，林卓然，等．地幔流体包裹体中多种固相充填物的发现及其意义．科学通报，1993,38(23)：2177-2180
215．徐九华，储雪蕾，邹一民，等．汉诺坝地幔捕虏体中的硫化物包裹体．科学通报，1998，43(13)：1438-1442．
216．徐九华，储雪蕾，谢玉玲，等．浙江新昌地幔岩捕虏体中的硫化物包裹体初步研究．地质论评，1999,4 5(6)：640-645
217．徐九华，谢玉玲，储雪蕾，等．中国东部地幔岩中的硫化物成分．矿床地质，2002,21(增)：1060-1063
218．储雪蕾，徐九华，赵善仁．地幔矿物中硫化物熔体包裹体的成因．地球物理学报，1998,4(增)：153-161
219.Guo J F,Griffin W L,O'Reilly S Y.Geochemistry and Origin of Sulphide Minerals in Mantle Xenoliths:Qilin,Southeastern China.Journal of Petrology,1999.40(7):1125-1149
220.Wells P R A.Pyroxene thermometry in simple and complex systems.Contrib.Mineral.Petrol,1977,62:129-139
221.Sachteben T,Seek H A.Chemical control of Al-solubility in orthopyroxene and its implications on pyroxene geochermometry.Contrib.Mineral.Petrol,1981,78:157-165
222. Brey, G, K(?)hler, T., 1990. Geochermobarometry in four-phase iherzolites.Ⅱ: New thermobarometers and practical assessment of existing thermobarometers. J.Petrol, 31, 1352-1378.
223. O'Reilly S Y, Griffin W L. 4-D lithosphere mapping: methodology and example. Tectonophysics, 1996, 262(1):3-18
224. McDonough W F, Sun S S. The composition of the Earth. Chem. Geol., 1995,120: 223-253
225. Claude T C. Lithosphere peridotites of the Kaapvaal Craton. Earth and Planetary Science Letters, 1993,120:13-29
226. Griffin W L, O'Reilly S Y and Ryan C G. The composition and origin of sub-continental lithospheric mantle. In Mantle Petrology: Field observations and high-pressure experimentation: A tribute to Francis R. (Joe) Boyd (eds. Fei Y, Berka C M and Mysen B O). The Geochemical Society, 1999(Special Publication), 6:13-45
227. Boyd F R. Origin of peridotite xenoliths: major element consideration. In high pressure and high temperature research on lithosphere and mantle materials (eds. Ranalli G, Ricci Lucchi F, Ricci C A, et al). University of Siena, Siena, 1996, 89-106
228. Boyd F R, Pearson D G, Nixon P H, et al. Low-calcium garnet harzburgites from southern Africa: their relations to craton structure and diamond crystallization. Contrib. Mineral. Petrol. 1993,113:352-366
229. Lee C T, Rudnick R L. Compositionally stratified cratonic lithosphere: petrology and geochemistry of peridotite xenoliths from the Labait volcano, Tanzania. In: Gurney J J, Gurney J L, Pascoe M D, et al(Eds.), The P H Nixon Volume. Proceedings Ⅶth International Kimberlite Conference. Red Roof Design, Cape Town, 1999,503-521
230. Sun S S, Mcdonough W F. Chemical and isotopic systematics of oceanic basalts: implications for mantle composition and processes. In: Saunders A D & Norry M J (eds). Magmatism in the Ocean Basins.Geological Society of London(Special Publication),42, 1989, 314-345
231. Johnson K T M, Dick H J B, Shimizu N. Melting in the oceanic upper mantle: An ion microprobe study of diopside in abyssal peridotites. J.Geophys.Res, 1990, 95: 2661-2678
232. Norman M D. Melting and metasomatism in the continental lithosphere: laser ablation ICPMS analysis of minerals in spinel lherzolites from eastern Australia. Contribution to Mineralogy and Petrology, 1998, 130,240-255
233. Wulff-Pedersen E, Neumann E R, Jensen B B. The upper mantle under La Palma, Canary Island: Formation of Si-K-Na-rich melt and its importance as a metasomatic agent. Comtrib.Mineral.Petrol, 1996,125: 113-139
234. Zangana N A, Downes H, Thirlwall M F, et al. Geochemical variation in peridotite xenoliths and their constituent clinopyroxenes from Ray Pic (?)French Massif Central.: implications for the composition of the shallow lithospheric mantle. Chem. Geol, 1999,153, 11-35
235. Meen J K. Mantle metasomatism and carbonates: an experimental study of a complex relationship. Geol. Soc. Am. (SpecPap), 1987,215:91-100
236. Yaxley G M, Green D H, Kamenetsky V. Carbonatite metasomatism in the southeastern Australia lithosphere.J Petrol,1998,39:1917-1930
237.Coltorti M,Bonadiman C,Hinton R W,et al.Carbonatite metasomatism of the oceanic upper mantle:evidence from clinopyroxenes and glasses in ultramafic xenoliths of Grande Comore,Indian Ocean.J.Petrol.,1999,40:133-165
238.Green D H.Experimental melting studies on a model upper mantle composition at high pressure under watersaturated and water-unsaturated conditions.Earth and Planetary Science Letters,1973 19,37-55
239.Green D H,Wallace M E.Mantle metasomatism by ephemeral carbonatite melts.Nature,1988,336,459-462
240．李天福，马鸿文，白志民．汉诺坝玄武岩的地球化学特征及成因模式．岩石矿物学杂志，1999， 18(3)：217-228
241.Palme H,O'Neill H St C.Cosmochemical estimates of mantle composition.In:Carlson R W(ed.).Treatise on Geochemistry:the mantle and core.Elsevier,2004,2:1-38
242.Bennett V C,Nutman A P,East T M.Constraints on mantle evolution from 187Os/188Os isotopic compositions of Archean ultramafic rocks from southern West Greenland (3.8Ga) and Western Australia (3.46Ga).Geochimica et Cosmochimica Acta,2002,66(14):2615-2630
243．支霞臣，Reisberg L，徐夕生．安徽女山幔源橄榄岩捕虏体Re-Os同位素地球化学．中国科学技术大学学报,2007,37(8)：945-952
244.Smoliar M I,Walker R J,Morgan J W.Re-Os ages of group ⅡA,ⅡA,IVB iron meteorites.Science,1996,271:1099-1102
245．徐义刚．岩石圈的热-机械侵蚀和化学侵蚀与岩石圈减薄．矿物岩石地球化学通报，1999，18(1)：1-5
246.Bird P.Initiation of intracontinental subduction in the Himalayas.Journal of Geophysics Research,1978,83(310):4975-4987
247．高山，金振民．拆沉作用(Delamination)及其壳-幔演化动力学意义．地质科技情报，1997，16(1)：1-9
248．高山，张本仁，金振民．秦岭-大别造山带下地壳拆沉作用．中国科学(D辑)，1999，29(6)：532-541
249．郑建平，孙敏，路凤香，等．信阳基性麻粒岩捕掳体及其华北南缘早中生代下地壳性质．岩石学报,2005,21(1)：91-98
250.Zhai M G,Fan Q C,Zhang H F,et al.Lower crustal processes leading to Mesozoic lithospheric thinning beneath eastern North China:underplating,replacement and delamination.Lithos,2007,96:36-54
251.Zheng J P,Griffin W L,O'Reilly S Y,et al.U-Pb and Hf-Isotope analysis of zircons in mafic xenoliths from Fuxian kimberlites:evolution of the lower crust beneath the North China Craton.Contribution to Mineralogy and Petrology,2004,148:79-103
252．侯贵廷，穆治国．华北克拉通晚前寒武纪镁铁质岩墙群K-Ar年龄及地质意义．华北地质矿产杂志，1994，9(3)：267-270
253．邵济安，张履桥，李大明．华北克拉通元古代的三次伸展事件．岩石学报,2002，18(2)：152-160
254．陆松年，李怀坤，李惠民，等．华北克拉通南缘龙王石童碱性花岗岩U-Pb年龄及其地质意义．地质通报，2003,22(12)：762-768
255．李宏基，李崇辉，杜利林．河北平山深熔伟晶岩锆石成因及SHRIPMP U-Pb年龄．自然科学进展，2004，14(17)：774-768
256.Zheng J P,Griffin W L,O'Reilly S Yet al.Zircons in mantle xenoliths record the Triassic Yangtze-North China continental collision.Earth Planetary Science Letters,2006,247:130-142
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