班公湖-怒江缝合带西段阿翁错复式岩体的岩浆混合成因:地球化学、年代学和暗色微粒包体证据
|
摘要
阿翁错复式岩体位于班公湖-怒江缝合带西段,是班公湖-怒江特提斯洋俯冲消减,造山过程中岩浆响应的重要组成部分,以广泛发育暗色微粒包体和岩浆混合、不协调现象为特征。本文以阿翁错复式岩体为研究对象,对寄主岩和暗色微粒包体开展了系统的地质学、地球化学和锆石U-Pb年代学研究,探讨了阿翁错复式岩体的岩浆混合成因。暗色微粒包体塑性变形特征明显,与寄主岩呈截然或渐变接触,偶见反向脉发育,包体具细-中粗粒结构,含斜长石、钾长石、角闪石、暗色镶边石英等斑晶,偶见角闪石斑晶横跨包体和寄主岩,在包体及包体周围寄主岩中见长柱状斜长石、角闪石和针状磷灰石等结构特征,表明暗色微粒包体为岩浆混合作用的产物。寄主岩与包体均为准铝质、钙碱性-高钾钙碱性系列岩石,主要氧化物含量在Harker图解上具有良好的线性关系,稀土元素配分曲线图和微量元素蛛网图具有高度一致性,表明二者具有强烈的地球化学亲源关系,且经历了相似的岩浆演化过程。寄主岩和暗色微粒包体的成岩年龄分别为109. 1±1. 0Ma和107. 4±0. 7Ma,岩浆混合作用发生在早白垩世晚期,处于班公湖-怒江特提斯洋由弧-陆碰撞向陆陆碰撞的转换阶段即软碰撞阶段。研究表明,在班公湖-怒江特提斯洋向北向羌塘地块之下俯冲的背景下,洋壳脱水,引起上覆地幔楔发生部分熔融,形成镁铁质岩浆,镁铁质岩浆向上运移,并底侵于壳-幔边界,引发下地壳物质发生部分熔融,形成长英质岩浆,当镁铁质岩浆从底部注入长英质岩浆房时,镁铁质岩浆快速冷凝,形成部分色率高、粒度细,具冷凝边的包体,与寄主岩呈截然型接触,随着端元岩浆之间的温差逐渐降低,包体色率降低,粒度变大,与寄主岩呈渐变过渡。
Located at the western part of Bangong Co-Nujiang Suture Zone,the Awengcuo composite plutons are the important part result in the magmatic response during the subduction of the Bangongco-Nujiang Tethys Ocean,and is featured by widely developed mafic microgranular enclaves,the magma mingling and the magma incoordination phenomenon. Taking Awengcuo composite plutons as the research object,this paper conducts an in-depth study on the geological characteristics and geochronology of mafic microgranular enclave and its formation mechanism. Mafic microgranular enclave has obvious plastic deformation features,and has sharp or gradual contact with the host rock,presenting still a little reverse pulse development. With the structure of fine to medium-coarse,the enclave contains many phenocrysts such as plagioclase,potash feldspar,hornblende,and dark rimmed quartz. Besides,plagioclase phenocryst is occasionally found across the enclave and the host rock,and long columnar plagioclase,hornblende,acicular apatite are also existed in the enclave and the host rock. All of them show that mafic microgranular enclave is produced by magma mixing. Host rock and MMEs are transitional rock such as quasi-aluminum,high-calcium alkaline-potassium kaolin series,and the main oxide content in the Harker diagram has a good linear relationship. Rare earth element distribution curve and normalized spidergram for trace element primitive mantle are with high degree of consistency. It shows that there is a strong geophysical relationship between the two groups,and experience the similar magmatic evolution process. A good linear relationship is showed between the host rock and inclusions in the denominator covariant map of the principle and trace elements. And their relationship is closely related to the magmatic mixing. Both of them contain a lot of large ion lithophile elements such as Rb,K,U,Th,and lack high field strenghth elements Nb,Ta,P,Ti. Dark Microgranular is low-silicon,but rich with Mg,Fe,Ca,The ratio of Nb/Ta is 17. 6,indicating that the original magma of the inclusions may be derived from the mantle wedge by fluid of subduction zone. While the host rock is relatively high in silicon and with lower Mg,Fe and Ca,Nb/Ta ratio is 9. 85,indicating that the host rock is the product of mantle-derived magma mixed with the molten lower crust magma,mainly with molten lower crust magma. The LA-ICP-MS single-zircons U-Pb dating demonstrates that the magmatic age is 109. 1 ± 1. 0 Ma for the host rock and 107. 4 ± 0. 7 Ma for the enclave. The two ages are basically the same,suggesting that the mixing event took place during the period of Early Cretaceous,during the soft collision phrase which the Bangong Co-Nujiang Tethys Ocean is transitional from the ocean-continent subduction to continent-continent subduction. Research shows that during BangongcoNujiang Tethyan Oceanic plate north-forward subduction to the Qiangtang block,the dehydration of oceanic crust leads to the partial melting of the overlain mantle wedge,and produces mafic magma. The mafic magma transfers upward and eventually intrudes into crust-mantle boundary,which causes the partial melting of the lower crustal materials and forms felsic magma. When the mafic magma flows at the bottom into the felsic magma chamber,it will condensates rapidly and become some enclave with high color ratio,fine granularity and condensation rim. Such enclave is in sharp contact with the host rock,while with the gradually declining temperature between end-member magmas,the color ratio of the enclave is becoming lower and its granularity bigger,then the enclave has a gradational contact with the host rock.
Located at the western part of Bangong Co-Nujiang Suture Zone,the Awengcuo composite plutons are the important part result in the magmatic response during the subduction of the Bangongco-Nujiang Tethys Ocean,and is featured by widely developed mafic microgranular enclaves,the magma mingling and the magma incoordination phenomenon. Taking Awengcuo composite plutons as the research object,this paper conducts an in-depth study on the geological characteristics and geochronology of mafic microgranular enclave and its formation mechanism. Mafic microgranular enclave has obvious plastic deformation features,and has sharp or gradual contact with the host rock,presenting still a little reverse pulse development. With the structure of fine to medium-coarse,the enclave contains many phenocrysts such as plagioclase,potash feldspar,hornblende,and dark rimmed quartz. Besides,plagioclase phenocryst is occasionally found across the enclave and the host rock,and long columnar plagioclase,hornblende,acicular apatite are also existed in the enclave and the host rock. All of them show that mafic microgranular enclave is produced by magma mixing. Host rock and MMEs are transitional rock such as quasi-aluminum,high-calcium alkaline-potassium kaolin series,and the main oxide content in the Harker diagram has a good linear relationship. Rare earth element distribution curve and normalized spidergram for trace element primitive mantle are with high degree of consistency. It shows that there is a strong geophysical relationship between the two groups,and experience the similar magmatic evolution process. A good linear relationship is showed between the host rock and inclusions in the denominator covariant map of the principle and trace elements. And their relationship is closely related to the magmatic mixing. Both of them contain a lot of large ion lithophile elements such as Rb,K,U,Th,and lack high field strenghth elements Nb,Ta,P,Ti. Dark Microgranular is low-silicon,but rich with Mg,Fe,Ca,The ratio of Nb/Ta is 17. 6,indicating that the original magma of the inclusions may be derived from the mantle wedge by fluid of subduction zone. While the host rock is relatively high in silicon and with lower Mg,Fe and Ca,Nb/Ta ratio is 9. 85,indicating that the host rock is the product of mantle-derived magma mixed with the molten lower crust magma,mainly with molten lower crust magma. The LA-ICP-MS single-zircons U-Pb dating demonstrates that the magmatic age is 109. 1 ± 1. 0 Ma for the host rock and 107. 4 ± 0. 7 Ma for the enclave. The two ages are basically the same,suggesting that the mixing event took place during the period of Early Cretaceous,during the soft collision phrase which the Bangong Co-Nujiang Tethys Ocean is transitional from the ocean-continent subduction to continent-continent subduction. Research shows that during BangongcoNujiang Tethyan Oceanic plate north-forward subduction to the Qiangtang block,the dehydration of oceanic crust leads to the partial melting of the overlain mantle wedge,and produces mafic magma. The mafic magma transfers upward and eventually intrudes into crust-mantle boundary,which causes the partial melting of the lower crustal materials and forms felsic magma. When the mafic magma flows at the bottom into the felsic magma chamber,it will condensates rapidly and become some enclave with high color ratio,fine granularity and condensation rim. Such enclave is in sharp contact with the host rock,while with the gradually declining temperature between end-member magmas,the color ratio of the enclave is becoming lower and its granularity bigger,then the enclave has a gradational contact with the host rock.
引文
Altherr R and Siebel W.2002.I-type plutonism in a continental back-arc setting:Miocene granitoids and monzonites from the central Aegean Sea,Greece.Contributions to Mineralogy and Petrology,143(4):397-415
Barbarin B.2005.Mafic magmatic enclaves and mafic rocks associated with some granitoids of the central Sierra Nevada batholith,California:Nature,origin,and relations with the hosts.Lithos,80(1-4):155-177
Baxter S and Feely M.2002.Magma mixing and mingling textures in granitoids:Examples from the Galway granite,Connemara,Ireland.Mineralogy and Petrology,76(1-2):63-74
Belousova EA,Griffin WL,O’reilly SY and Fisher NI.2002.Igneous zircon:Trace element composition as an indicator of source rock type.Contributions to Mineralogy and Petrology,143:602-622
Bonin B.2004.Do coeval mafic and felsic magmas in post-collisional to within-plate regimes necessarily imply two contrasting,mantle and crustal,sources?A review.Lithos,78(1-2):1-24
Bonin B.2007.A-type granites and related rocks:Evolution of a concept,problems and prospects.Lithos,97(1-2):1-29
Boynton WV.1984.Geochemistry of the rare earth elements:Meteorite studies.In:Henderson P(ed.).Rare Earth Element Geochemistry.Amsterdam:Elsevier,63-114
Castro A.2013.Tonalite-granodiorite suites as cotectic systems:A review of experimental studies with applications to granitoid petrogenesis.Earth-Science Reviews,124:68-95
Champion DC and Bultitude RJ.2013.The geochemical and Sr-Nd isotopic characteristics of Paleozoic fractionated S-types granites of North Queensland:Implications for S-type granite petrogenesis.Lithos,162-163:37-56
Chappell BW and White AJR.1991.Restite enclaves and the restite model.In:Didier J and Barbarin B(eds.).Enclaves and Granite Petrology.Amsterdam:Elsevier,375-381
Chen B,Liu CQ and Tian W.2006.Magma-mixing between mantle-and crustal-derived melts in the process of Mesozoic magmatism,Taihangshan:Constraints from petrology and geochemistry.Earth Science Frontiers,13(2):140-147(in Chinese with English abstract)
Chen GJ,Sun FY,Li BL,Wang G,Qian Y,Xu QL and Liu GC.2014.Geochemistry and petrogenesis of Gouli mafic enclaves and their host rocks in eastern Kunlun.Journal of Jilin University(Earth Science Edition),44(3):892-904(in Chinese with English abstract)
Chen GC,Pei XZ,Li RB,Li ZC,Liu CJ,Chen YX,Xu T and Zhang YM.2016.Genesis of magma mixing and mingling of Xiangjiananshan granite batholith in the eastern section of East Kunlun orogen:Evidence from mafic microgranular enclaves(MMEs).Earth Science Frontiers,23(4):226-240(in Chinese with English abstract)
Didier J.1973.Granites and Their Enclaves:The Bearing of Enclaves on the Origin of Granites.Amsterdam:Elsevier,1-393
Ding S,Tang JX,Zheng WB,Yang C,Zhang Z,Wang Q and Wang YY.2017.Geochronology and geochemistry of Naruo porphyry Cu(Au)deposit in Duolong ore-concentrated area,Tibet,and their geological significance.Earth Science,42(1):1-23(in Chinese with English abstract)
Dong GC,Mo XX,Zhao ZD,Zhu DC,Wang LL,Chen T and Li B.2006.Magma mixing in middle part of Gangdise magma belt:Evidences from granitoid complex.Acta Petrologica Sinica,22(4):835-844(in Chinese with English abstract)
Du DD,Qu XM,Wang GH,Xin HB and Liu ZB.2011.Bidirectional subduction of the Middle Tethys oceanic basin in the west segment of Bangonghu-Nujiang suture,Tibet:Evidence from zircon U-Pb LAICPMS dating and petrogeochemistry of arc granites.Acta Petrologica Sinica,27(7):1993-2002(in Chinese with English abstract)
Eichelberger JC.1980.Vesiculation of mafic magma during replenishment of silicic magma reservoirs.Nature,288(5790):446-450
Feeley TC,Wilson LF and Underwood SJ.2008.Distribution and compositions of magmatic inclusions in the Mount Helen dome,Lassen Volcanic Center,California:Insights into magma chamber processes.Lithos,106(1-2):173-189
Frost TP and Mahood GA.1987.Field,chemical,and physical constraints on mafic-felsic magma interaction in the Lamarck granodiorite,Sierra Nevada,California.Geological Society of America Bulletin,99(2):272-291
Fu Q,Ge WS,Wen CS,Cai KQ,Li SF,Zhang ZW and Li XF.2011.Geochemistry and genesis of Michang granites and their dark microgranular enclaves in Guangxi.Acta Geoscientica Sinica,32(3):293-303(in Chinese with English abstract)
Gu FH,Zhang YM,Liu RP,Zheng L and Sun X.2015.Magma mixing and mingling of the Shadegai granite in Inner Mongolia:Evidence from petrography,mineral chemistry and geochronology.Acta Petrologica Sinica,31(5):1374-1390(in Chinese with English abstract)
Hao BW.2012.Discovery,genesis and tectonic significance of the LatePaleozoic miarolitic K-feldspar granite in southern Xianghuangqi,Inner Mongolia.Journal of Jilin University(Earth Science Edition),42(2):269-284(in Chinese with English abstract)
Huang QS,Shi RD,Ding BH,Liu DL,Zhang XR,Fan SQ and Zhi XC.2012.Re-Os isotopic evidence of MOR-type ophiolite from the Bangong Co for the opening of Bangong-Nujiang Tethys Ocean.Acta Petrologica et Mineralogica,31(4):465-478(in Chinese with English abstract)
Huppert EH and Sparks RSJ.1988.The generation of granitic magmas by intrusion of basalt into continental crust.Journal of Petrology,29(3):599-624
Jin XC and Yu KP.2003.Subduction factory and subduction recycling of continental material.Advance in Earth Sciences,18(5):737-744(in Chinese with English abstract)
Jochum KP,Mc Donough WF,Palme H and Spettel B.1989.Compositional constraints on the continental lithospheric mantle from trace elements in spinel peridotite xenoliths.Nature,340(6234):548-550
Jung S and Pfnder JA.2007.Source composition and melting temperatures of orogenic granitoids:Constraints from CaO/Na2O,Al2O3/Ti O2and accessory mineral saturation thermometry.European Journal of Mineralogy,19(6):859-870
Kang L,Li YJ,Zhang B,Zhang HW and Wang JN.2009.Petrographic evidence for magma mixing of Xiaerpu granite in West Junggar,Xinjiang.Acta Petrologica et Mineralogica,28(5):423-432(in Chinese with English abstract)
Kapp P,Yin A,Harrison TM and Lin D.2005.Cretaceous-Tertiary shortening,basin development,and volcanism in central Tibet.Geological Society of America Bulletin,117(7-8):865-878
Kumar S and Rino V.2006.Mineralogy and geochemistry of microgranular enclaves in Palaeoproterozoic Malanjkhand granitoids,central India:Evidence of magma mixing,mingling,and chemical equilibration.Contributions to Mineralogy and Petrology,152(5):591-609
Kumar S and Pieru T.2010.Petrography and major elements geochemistry of microgranular enclaves and Neoproterozoic granitoids of South Khasi,Meghalaya:Evidence of magma mixing and alkali diffusion.Journal of the Geological Society of India,76(4):345-360
Lei CY,Li ZJ,Zhang Z,Hu ZH,Wang HX and Song JL.2012.Geochemical characteristics and geodynamic significance of the granites in the Ga’erqiong Cu-Au deposit,Tibet.Acta Geoscientica Sinica,33(4):601-612(in Chinese with English abstract)
Lei CY,Wu JL,Yin XK,Liu W,Wang B,Li W,Yuan HY,Zhang W,Yin T and Pei YL.2018.New discovery of the diorite porphyry dyke in the Shamuluo formation in western segment of the BangongcoNujiang suture zone and its geological significance.Bulletin of Mineralogy,Petrology and Geochemistry,37(2):250-259(in Chinese with English abstract)
Lei CY,Wu JL,Yin XK,Liu W,Wang B,Li W,Yuan HY,Zhang W,Yin T and Pei YL.2019.Petrogenesis of intermediate-acid intrusive rocks in Awengcuo area in the west segment of the BangongcoNujiang Suture,Tibet,and its instructions to the regional tectonic evolution.Geotectonica et Metallogenia,43(1):168-185(in Chinese with English abstract)
Lei M,Chen JL,Xu JF and Zeng YC.2015.Geochemistry of early Late Cretaceous Gaerqiong high-Mg#diorite porphyry in midnorthern Lhasa terrane:Partial melting of delaminated lower continental crust?Geological Bulletin of China,34(2-3):337-346(in Chinese with English abstract)
Li CN.1999.Discovery for Precambrian magmatic mixed zone from northeastern Jiangxi Province and their geological significance.Earth Science Frontiers,6(4):331-337(in Chinese with English abstract)
Li FQ,Liu ZB,Tang JX,Song Y,Gao K,Li HF,Zhao ZQ and Teng L.2018.Petrogenesis of granite porphyry in mariaicuo area,Shuanghu County,Tibet,and constraints on the evolution in the middle section of Bangonghu-Nujiang suture zone.Earth Science,43(4):1051-1069(in Chinese with English abstract)
Li GM,Zhang XN,Qin KZ,Sun XG,Zhao JX,Yin XB,Li JX and Yuan HS.2015.The telescoped porphyry-high sulfidation epithermal Cu(-Au)mineralization of Rongna deposit in Duolong ore cluster at the southern margin of Qiangtang Terane,Central Tibet:Integrated evidence from geology,hydrothermal alteration and sulfide assemblages.Acta Petrologica Sinica,31(8):2307-2324(in Chinese with English abstract)
Li HL,Gao C,Li ZH,Zhang Z,Peng ZM and Guan JL.2016.Age and tectonic significance of Jingzhushan Formation in Bangong Lake area,Tibet.Geotectonica et Metallogenia,40(4):663-673(in Chinese with English abstract)
Li JX,Qin KZ and Li GM.2006.Basic characteristics of gold-rich porphyry copper deposits and their ore sources and evolving processes of high oxidation magma and ore-forming fluid.Acta Petrologica Sinica,22(3):678-688(in Chinese with English abstract)
Li JX.2008.Geochronology,petrology and metallogeneses of high oxidized magma-hydrothermal fluid of Duobuza gold-rich porphyry copper deposit in Bangonghu belt,Northern Tibet.Ph.D.Dissertation.Beijing:Institute of Geology and Geophysics,Chinese Academy of Sciences 1-224(in Chinese with English summary)
Li JX,Qin KZ,Li GM,Xiao B,Zhao JX,Cao MJ and Chen L.2013.Petrogenesis of ore-bearing porphyries from the Duolong porphyry CuAu deposit,central Tibet:Evidence from U-Pb geochronology,petrochemistry and Sr-Nd-Hf-O isotope characteristics.Lithos,160-161:216-227
Li XH,Zhou HW,Liu Y,Lee CY,Chen ZH,Yu JS and Gui XT.2000.Mesozoic shoshonitic intrusives in the Yangchun Basin,western Guangdong,and their tectonic significance:Ⅰ.Petrology and isotope geochronology.Geochimica,29(6):513-520(in Chinese with English abstract)
Lin B,Chen YC,Tang JX,Wang Q,Song Y,Yang C,Wang WL,He W and Zhang LJ.2017a.40Ar/39Ar and Rb-Sr ages of the Tiegelongnan porphyry Cu-(Au)deposit in the Bangong Co-Nujiang metallogenic belt of Tibet,China:Implication for generation of super-large deposit.Acta Geologica Sinica,91(2):602-616
Lin B,Tang JX,Chen YC,Song Y,Hall G,Wang Q,Yang C,Fang X,Duan JL,Yang HH,Liu ZB,Wang YY and Feng J.2017b.Geochronology and genesis of the Tiegelongnan porphyry Cu(Au)deposit in Tibet:Evidence from U-Pb,Re-Os dating and Hf,S,and H-O isotopes.Resource Geology,67(1):1-21
Lin B,Tang JX,Song Y,Wang Q,Cao HW,Baker M,Zhang LJ and Li YB.2017.Petrogeochemistry and SHRIMP dating of Ga’erqin pillow basalt in Duolong,Northern Tibet.Acta Geoscientica Sinica,38(5):702-710(in Chinese with English abstract)
Lin B,Tang JX,Chen YC,Baker M,Song Y,Yang HH,Wang Q,He W and Liu ZB.2019.Geology and geochronology of Naruo large porphyry-breccia Cu deposit in the Duolong district,Tibet.Gondwana Research,66:168-182
Liu YS,Hu ZC,Gao S,Günther D,Xu J,Gao CG and Chen HH.2008.In situ analysis of major and trace elements of anhydrous minerals by LA-ICP-MS without applying an internal standard.Chemical Geology,257(1-2):34-43
Liu YS,Hu ZC,Zong KQ,Gao CG,Gao S,Xu J and Chen HH.2010.Reappraisement and refinement of zircon U-Pb isotope and trace element analyses by LA-ICP-MS.Chinese Science Bulletin,55(15):1535-1546
Ma CQ,Yang KG,Tang ZH and Li ZT.1994.Magma-Dynamics of Granitoids Theory,Method and A Case Study of the Eastern Hubei Granitoids.Wuhan:China University of Geosciences Press(in Chinese)
Ma LT,Zhang ZC,Dong SY,Zhang S,Zhang DY and Huang H.2010.Geology and geochemistry of the Yingmailai granitic intrusion in the Southern Tianshan and its implications.Earth Science(Journal of China University of Geosciences),35(6):908-920(in Chinese with English abstract)
Maas R,Nicholls IA and Legg C.1997.Igneous and metamorphic enclaves in the S-type Deddick granodiorite,Lachlan Fold Belt,SEAustralia:Petrographic,geochemical and Nd-Sr isotopic evidence for crustal melting and magma mixing.Journal of Petrology,38(7):815-841
Mc Donough WF,Sun SS,Ringwood AE,Jagoutz E and Hofmann AW.1992.Potassium,rubidium,and cesium in the Earth and Moon and the evolution of the mantle of the Earth.Geochimica et Cosmochimica Acta,56(3):1001-1012
Mo XX.2011.Magma and magmatic/igneous rocks:A lithoprobe into the deep earth and records of the earth’s evolution.Chinese Journal of Nature,33(5):255-259(in Chinese with English abstract)
Montel JM and Vielzeuf D.1997.Partial melting of metagreywackes,PartⅡ.Compositions of minerals and melts.Contributions to Mineralogy and Petrology,128(2-3):176-196
Noyes HJ,Frey FA and Wones DR.1983.A tale of two plutons:Geochemical evidence bearing on the origin and differentiation of the Red Lake and Eagle Peak plutons,Central Sierra Nevada,California.The Journal of Geology,91(5):487-509
Paterson SR,Pignotta GS and Vernon RH.2004.The significance of microgranitoid enclave shapes and orientations.Journal of Structural Geology,26(8):1465-1481
Pearce JA.1996.Sources and settings of granitic rocks.Episodes,19(4):120-125
Perugini D,Poli G,Christofides G and Eleftheriadis G.2003.Magma mixing in the Sithonia plutonic complex,Greece:Evidence from mafic microgranular enclaves.Mineralogy and Petrology,78(3-4):173-200
Qi YQ,Hu RZ,Liu S and Tian JJ.2008.Review on magma mixing and mingling.Bulletin of Mineralogy,Petrology and Geochemistry,27(4):409-416(in Chinese with English abstract)
Qiangba ZX,Xie YW,Wu YW,Xie CM,Li QL and Qiu JQ.2009.Zircon SIMS U-Pb dating and its significance of cumulate gabbro from Dengqen ophiolite,eastern Tibet,China.Geological Bulletin of China,28(9):1253-1258(in Chinese with English abstract)
Qiangba ZX,Wu H,Gesang WD,Ciren OZ,Basang DZ,Qiong D and Niu DW.2016.Early Cretaceous magmatism in Dongqiao,Tibet:Implications for the evolution of the Bangong-Nujiang Ocean and crustal growth in a continent-continent collision zone.Geological Bulletin of China,35(5):648-666(in Chinese with English abstract)
Qiu JS,Wang RQ,Zhao JL and Yu SB.2015.Petrogenesis of the Early Jurassic gabbro-granite complex in the middle segment of the Gangdese belt and its implications for tectonic evolution of NeoTethys:A case study of the Dongga pluton in Xi’gaze.Acta Petrologica Sinica,31(22):3569-3580(in Chinese with English abstract)
Qu XM,Wang RJ,Xin HB,Zhao YY and Fan XT.2009.Geochronology and geochemistry of igneous rocks related to the subduction of the Tethys oceanic plate along the Bangong Lake arc zone,the western Tibetan Plateau.Geochimica,38(6):523-535(in Chinese with English abstract)
Ren JS,Niu BG and Liu ZG.1999.Soft collision,superposition orogeny and polycyclic suturing.Earth Science Frontiers,6(3):85-93(in Chinese with English abstract)
Rickwood PC.1989.Boundary lines within petrologic diagrams which use oxides of major and minor elements.Lithos,22(4):247-263
Rudnick RL and Gao S.2003.Composition of the continental crust.In:Rudniek RL(ed.).Treatise on Geochemistry.Amsterdam:Elsevier,1-64
Rushmer T.1991.Partial melting of two amphibolites:Contrasting experimental results under fluid-absent conditions.Contributions to Mineralogy and Petrology,107(1):41-59
Shamberger PJ and Garcia MO.2007.Geochemical modeling of magma mixing and magma reservoir volumes during early episodes of Kīlauea Volcano’s Pu‘u‘‘ōeruption.Bulletin of Volcanology,69(4):345-352
Shellnutt JG,Jahn BM and Dostal J.2010.Elemental and Sr-Nd isotope geochemistry of microgranular enclaves from peralkaline A-type granitic plutons of the Emeishan large igneous province,SW China.Lithos,119(1):34-46
Shi RD,Griffin WL,O’Reilly SY,Huang QS,Zhang XR,Liu DL,Zhi XC,Xia QX and Ding L.2012.Melt/mantle mixing produces podiform chromite deposits in ophiolites:Implications of Re-Os systematics in the Dongqiao Neo-Tethyan ophiolite,northern Tibet.Gondwana Research,21(1):194-206
Song B,Zhang YH,Wan YS and Jian P.2002.Mount making and procedure of the SHRIMP dating.Geological Review,48(Suppl.):26-30(in Chinese with English abstract)
Song Y,Qu XM,Xin HB,Wang ZY and Du DD.2013.The crustal carbon cycling in the Late Cretaceous extension of Bangong Lake arc zone in the Xizang(Tibetan)Plateau.Geological Review,59(2):225-233(in Chinese with English abstract)
Song Y,Yang HH,Lin B,Liu ZB,Wang Q,Gao K,Yang C and Fang X.2017.The preservation system of epithermal deposits in South Qiangtang terrane of central Tibetan Plateau and its significance:Acase study of the Tiegelongnan superlarge deposit.Acta Geoscientica Sinica,38(5):659-669(in Chinese with English abstract)
Song Y,Yang C,Wei SG,Yang HH,Fang X and Lu HT.2018.Tectonic control,reconstruction and preservation of the Tiegelongnan porphyry and epithermal overprinting Cu(Au)deposit,Central Tibet,China.Minerals,8(9):398
Spring L,Bussy F,Vannay J C,Huon S and Cosca MA.1993.Early Permian granitic dykes of alkaline affinity in the Indian High Himalaya of upper Lahul and SE Zanskar:Geochemical characterization and geotectonic implications.Geological Society,London,Special Publications,74(1):251-264
Stampfli GM and Borel GD.2002.A plate tectonic model for the Paleozoic and Mesozoic constrained by dynamic plate boundaries and restored synthetic oceanic isochrons.Earth and Planetary Science Letters,196(1-2):17-33
Tang JX,Sun XG,Ding S,Wang Q,Wang YY,Yang C,Chen HQ,Li YB,Li YB,Wei LJ,Zhang Z,Song JL,Yang HH,Duan JL,Gao K,Fang X and Tan JY.2014a.Discovery of the epithermal deposit of Cu(Au-Ag)in the Duolong ore concentrating area,Tibet.Acta Geoscientica Sinica,35(1):6-10(in Chinese with English abstract)
Tang JX,Wang Q,Yang C,Ding S,Lang XH,Liu HF,Huang Y,Zheng WB,Wang LQ,Gao YM,Feng J,Duan JL,Song Y,Wang YY,Lin B,Fang X,Zhang Z and Yang HH.2014b.Two porphyryepithermal deposit metallogenic subseries in Tibetan Plateau:Practice of“absence prospecting”deposit metallogenic series.Mineral Deposits,33(6):1151-1170(in Chinese with English abstract)
Tang JX,Song Y,Wang Q,Lin B,Yang C,Guo N,Fang X,Yang HH,Wang YY,Gao K,Ding S,Zhang Z,Duan JL,Chen HQ,Su DK,Feng J,Liu ZB,Wei SG,He W,Song JL,Li YB and Wei LJ.2016.Geological characteristics and exploration model of the Tiegelongnan Cu(Au-Ag)deposit:The first ten million tons metal resources of a porphyry-epithermal deposit in Tibet.Acta Geoscientica Sinica,37(6):663-690(in Chinese with English abstract)
Tang JX,Wang Q,Yang HH,Gao X,Zhang ZB and Zou B.2017.Mineralization,exploration and resource potential of porphyry-skarnepithermal copper polymetallic deposits in Tibet.Acta Geoscientica Sinica,38(5):571-613(in Chinese with English abstract)
Troll VR and Schmincke HU.2002.Magma mixing and crustal recycling recorded in ternary feldspar from compositionally zoned peralkaline ignimbrite‘A’,Gran Canaria,Canary Islands.Journal of Petrology,43(2):243-270
Vernon RH.1983.Restite,xenoliths and microgranitoid enclaves in granites.Journal and Proceedings,Royal Society of New South Wales,116(3):77-103
Vernon RH.2014.Microstructures of microgranitoid enclaves and the origin of S-type granitoids.Australian Journal of Earth Sciences,61(2):227-239
Wang BD,Wang LQ,Chung SL,Chen JL,Yin FG,Liu H,Li XB and Chen LK.2016.Evolution of the Bangong-Nujiang Tethyan Ocean:Insights from the geochronology and geochemistry of mafic rocks within ophiolites.Lithos,245:18-33
Wang DZ,Zhou XM,Xu XS and Yao YP.1992.On geneses of microgranitoid enclaves.Journal of Guilin College of Geology,12(3):235-241(in Chinese)
Wang DZ and Xie L.2008.Magma mingling:Evidence from enclaves.Geological Journal of China Universities,14(1):16-21(in Chinese with English abstract)
Wang Q,Lin B,Tang JX,Song Y,Li YB,Hou JF,Li YB and Wei LJ.2018.Diagenesis,lithogenesis and geodynamic setting of intrusions in Senadong area,Duolong district,Tibet.Earth Science,43(4):1125-1141(in Chinese with English abstract)
Wang T.2000.Origin of hybrid granitoids and the implications for continental dynamics.Acta Petrologica Sinica,16(2):161-168(in Chinese with English abstract)
Wang YW,Wang JB,Long LL,Zou T,Tang PZ and Wang LJ.2012.Type,indicator,mechanism,model and relationship with mineralization of magma mixing:A case study in North Xinjiang.Acta Petrologica Sinica,28(8):2317-2330(in Chinese with English abstract)
Wei SG,Song Y,Tang JX,Gao K,Feng J,Li YB and Hou L.2016.Geochronology,geochemistry and petrogenesis of quartz diorite porphyrite from the Sena copper(gold)deposit,Tibet.Geology in China,43(6):1894-1912(in Chinese with English abstract)
Wei SG,Tang JX,Song Y,Liu ZB,Wang Q,Lin B,He W and Feng J.2017a.Petrogenesis,zircon U-Pb geochronology and Sr-Nd-Hf isotopes of the intermediate-felsic volcanic rocks from the Duolong deposit in the Bangonghu-Nujiang suture zone,Tibet,and its tectonic significance.Acta Geologica Sinica,91(1):132-150(in Chinese with English abstract)
Wei SG,Tang JX,Song Y,Liu ZB,Wang Q,Lin B,Wang YY,Fang X,Yang HH and Feng J.2017b.Zircons LA-MC-ICP-MS U-Pb ages,petrochemical,petrological and its significance of the Potassic monzonitic granite porphyry from the Duolong ore concentrated district,Gaize County,Xizang(Tibet).Geological Review,63(1):189-206(in Chinese with English abstract)
Winther KT.1996.An experimentally based model for the origin of tonalitic and trondhjemitic melts.Chemical Geology,127(1-3):43-59
Wu YB and Zheng YF.2004.Genesis of zircon and its constraints on interpretation of U-Pb age.Chinese Science Bulletin,49(15):1554-1569
Xiao QH,Deng JF,Ma DQ,Hong DW,Mo XX,Lu XX,Li ZC,Wang XW,Ma CQ,Wu FY,Luo ZH and Wang T.2002.The Ways of Investigation on Granitoids.Beijing:Geological Publishing House(in Chinese)
Xu JF,Mei HJ,Yu XY,Bai ZH,Niu HC,Chen FR,Zheng ZP and Wang Q.2001.Adakites related to subduction in the northern margin of Junggar arc for the Late Paleozoic:Products of slab melting.Chinese Science Bulletin,46:684-688(in Chinese)
Yu JJ,Hou XG,Ge WC,Zhang YL and Liu JC.2013.Magma mixing genesis of the Early Permian Liulian pluton at the northeastern margin of the Jiamusi massif in NE China:Evidences from petrography,geochronology and geochemistry.Acta Petrologica Sinica,29(9):2971-2986(in Chinese with English abstract)
Zhang C,Liu CZ,Wu FY,Zhang LL and Ji WQ.2016.Geochemistry and geochronology of mafic rocks from the Luobusa ophiolite,South Tibet.Lithos,245:93-108
Zhang DQ.1981.The characteristics and origin of the dioritic inclusions in the Fangshan intrusion,Beijing.Geological Review,27(2):143-149(in Chinese with English abstract)
Zhang Q,Pan GQ,Li CD,Jin WJ and Jia XQ.2007.Granitic magma mixing versus basaltic magma mixing:New viewpoints on granitic magma mixing process:Some crucial questions on granite study(1).Acta Petrologica Sinica,23(5):1141-1152(in Chinese with English abstract)
Zhang Z,Fang X,Tang JX,Wang Q,Yang C,Wang YY,Ding S and Yang HH.2017.Chronology,geochemical characteristics of the Gaerqin porphyry copper deposit in the Duolong ore concentration area in Tibet and discussion about the identification of the lithoscaps and the possible epithermal deposit.Acta Petrologica Sinica,33(2):476-494(in Chinese with English abstract)
Zhao YJ,Yuan C,Zhou MF,Yan DP,Long XP and Li JG.2007.Geochemistry and petrogenesis of Laojungou and Mengtonggou granites in western Sichuan,China:Constraints on the nature of Songpan-Ganzi basement.Acta Petrologica Sinica,23(5):995-1006(in Chinese with English abstract)
Zhou WG,Xie HS,Liu YG,Zheng XG,Zhao ZD and Zhou H.2005.Dehydration melting of solid amphibolite at 2.0GPa:Effects of time and temperature.Science in China(Series D),48(8):1120-1133
Zhu DC,Mo XX,Zhao ZD,Niu Y,Wang LQ,Chu QH,Pan GT,Xu JF and Zhou CY.2010.Presence of Permian extension-and arc-type magmatism in southern Tibet:Paleogeographic implications.Geological Society of America Bulletin,122(7-8):979-993
陈斌,刘超群,田伟.2006.太行山中生代岩浆作用过程中的壳幔岩浆混合作用:岩石学和地球化学证据.地学前缘,13(2):140-147
陈广俊,孙丰月,李碧乐,王冠,钱烨,许庆林,刘国才.2014.东昆仑沟里地区暗色包体及其寄主岩石地球化学特征及成因.吉林大学学报(地球科学版),44(3):892-904
陈国超,裴先治,李瑞保,李佐臣,刘成军,陈有炘,徐通,张永明.2016.东昆仑东段香加南山花岗岩基的岩浆混合成因:来自镁铁质微粒包体的证据.地学前缘,23(4):226-240
丁帅,唐菊兴,郑文宝,杨超,张志,王勤,王艺云.2017.西藏拿若斑岩型铜(金)矿含矿岩体年代学、地球化学及地质意义.地球科学,42(1):1-23
董国臣,莫宣学,赵志丹,朱弟成,王亮亮,陈涛,李冰.2006.冈底斯岩浆带中段岩浆混合作用:来自花岗杂岩的证据.岩石学报,22(4):835-844
杜德道,曲晓明,王根厚,辛洪波,刘治博.2011.西藏班公湖-怒江缝合带西段中特提斯洋盆的双向俯冲:来自岛弧型花岗岩锆石U-Pb年龄和元素地球化学的证据.岩石学报,27(7):1993-2002
付强,葛文胜,温长顺,蔡克勤,李世富,张志伟,李小飞.2011.广西米场花岗岩及其暗色微粒包体的地球化学特征和成因分析.地球学报,32(3):293-303
顾枫华,章永梅,刘瑞萍,郑硌,孙玄.2015.内蒙古沙德盖花岗岩岩浆混合作用:岩相学、矿物化学和年代学证据.岩石学报,31(5):1374-1390
郝百武.2012.内蒙古镶黄旗南晚古生代晶洞钾长花岗岩杂岩的发现、岩石成因及其构造意义.吉林大学学报(地球科学版),42(2):269-284
黄启帅,史仁灯,丁炳华,刘德亮,张晓冉,樊帅权,支霞臣.2012.班公湖MOR型蛇绿岩Re-Os同位素特征对班公湖-怒江特提斯洋裂解时间的制约.岩石矿物学杂志,31(4):465-478
金性春,于开平.2003.俯冲工厂和大陆物质的俯冲再循环研究.地球科学进展,18(5):737-744
康磊,李永军,张兵,张洪伟,王军年.2009.新疆西准噶尔夏尔莆岩体岩浆混合的岩相学证据.岩石矿物学杂志,28(5):423-432
雷传扬,李志军,张志,胡正华,王红星,宋俊龙.2012.西藏尕尔穷铜金矿床花岗岩类的地球化学特征及其地球动力学意义.地球学报,33(4):601-612
雷传扬,吴建亮,尹显科,刘文,王波,李威,袁华云,张伟,尹滔,裴亚伦.2018.班公湖-怒江缝合带西段沙木罗组地层中闪长玢岩脉的发现及其地质意义.矿物岩石地球化学通报,37(2):250-259
雷传扬,吴建亮,尹显科,刘文,王波,李威,袁华云,张伟,尹滔,裴亚伦.2019.班公湖-怒江缝合带西段阿翁错地区中酸性侵入岩的成因及其对区域构造演化的指示.大地构造与成矿学,43(1):168-185
雷鸣,陈建林,许继峰,曾云川.2015.拉萨地体中北部尕尔穷晚白垩世早期高镁闪长玢岩地球化学特征指示:加厚下地壳的拆沉?地质通报,34(2-3):337-346
李昌年.1999.赣东北前寒武纪岩浆混合作用岩带的发现及其地质意义.地学前缘,6(4):331-337
李发桥,刘治博,唐菊兴,宋扬,高轲,李海峰,赵志强,滕磊.2018.西藏玛日埃错地区花岗斑岩岩石成因及其对班公湖-怒江缝合带中段演化的制约.地球科学,43(4):1051-1069
李光明,张夏楠,秦克章,孙兴国,赵俊兴,印贤波,李金祥,袁华山.2015.羌塘南缘多龙矿集区荣那斑岩-高硫型浅成低温热液Cu-(Au)套合成矿:综合地质、热液蚀变及金属矿物组合证据.岩石学报,31(8):2307-2324
李华亮,高成,李正汉,张璋,彭智敏,关俊雷.2016.西藏班公湖地区竟柱山组时代及其构造意义.大地构造与成矿学,40(4):663-673
李金祥,秦克章,李光明.2006.富金斑岩型铜矿床的基本特征、成矿物质来源与成矿高氧化岩浆-流体演化.岩石学报,22(3):678-688
李金祥.2008.班公湖带多不杂超大型富金斑岩铜矿床的成岩成矿年代学、岩石学及高氧化岩浆-流体-成矿作用.博士学位论文.北京:中国科学院地质与地球物理研究所,1-224
李献华,周汉文,刘颖,李寄嵎,陈正宏,于津生,桂训唐.2000.粤西阳春中生代钾玄质侵入岩及其构造意义:Ⅰ.岩石学和同位素地质年代学.地球化学,29(6):513-520
林彬,唐菊兴,宋扬,王勤,曹华文,Baker M,张乐骏,李玉彬.2017.藏北多龙矿集区尕尔勤枕状玄武岩地球化学及SHRIMP测年.地球学报,38(5):702-710
马昌前,杨坤光,唐仲华,李增田.1994.花岗岩类岩浆动力学:理论方法及鄂东花岗岩类例析.武汉:中国地质大学出版社
马乐天,张招崇,董书云,张舒,张东阳,黄河.2010.南天山英买来花岗岩的地质、地球化学特征及其地质意义.地球科学-中国地质大学学报,35(6):908-920
莫宣学.2011.岩浆与岩浆岩:地球深部“探针”与演化记录.自然杂志,33(5):255-259
齐有强,胡瑞忠,刘燊,田建吉.2008.岩浆混合作用研究综述.矿物岩石地球化学通报,27(4):409-416
强巴扎西,谢尧武,吴彦旺,解超明,李秋立,邱军强.2009.藏东丁青蛇绿岩中堆晶辉长岩锆石SIMS U-Pb定年及其意义.地质通报,28(9):1253-1258
强巴扎西,吴浩,格桑旺堆,次仁欧珠,巴桑顿珠,琼达,女达娃.2016.班公湖-怒江缝合带中段东巧地区早白垩世岩浆作用---对大洋演化和地壳增厚的指示.地质通报,35(5):648-666
邱检生,王睿强,赵姣龙,喻思斌.2015.冈底斯中段早侏罗世辉长岩-花岗岩杂岩体成因及其对新特提斯构造演化的启示:以日喀则东嘎岩体为例.岩石学报,31(12):3569-3580
曲晓明,王瑞江,辛洪波,赵元艺,樊兴涛.2009.西藏西部与班公湖特提斯洋盆俯冲相关的火成岩年代学和地球化学.地球化学,38(6):523-525
任纪舜,牛宝贵,刘志刚.1999.软碰撞、叠覆造山和多旋回缝合作用.地学前缘,6(3):85-93
宋彪,张玉海,万渝生,简平.2002.锆石SHRIMP样品靶制作、年龄测定及有关现象讨论.地质论评,48(增):26-30
宋扬,曲晓明,辛洪波,王志云,杜德道.2013.西藏班公湖岛弧带晚白垩世地壳伸展期间碳的壳内循环.地质论评,59(2):225-233
宋扬,杨欢欢,林彬,刘治博,王勤,高轲,杨超,方向.2017.青藏高原羌塘地体南缘浅成低温热液成矿系统的保存机制及其重要意义---以铁格隆南超大型矿床为例.地球学报,38(5):659-669
唐菊兴,孙兴国,丁帅,王勤,王艺云,杨超,陈红旗,李彦波,李玉彬,卫鲁杰,张志,宋俊龙,杨欢欢,段吉琳,高轲,方向,谭江云.2014a.西藏多龙矿集区发现浅成低温热液型铜(金银)矿床.地球学报,35(1):6-10
唐菊兴,王勤,杨超,丁帅,郎兴海,刘鸿飞,黄勇,郑文宝,王立强,高一鸣,冯军,段吉琳,宋杨,王艺云,林彬,方向,张志,杨欢欢.2014b.青藏高原两个斑岩-浅成低温热液矿床成矿亚系列及其“缺位找矿”之实践.矿床地质,33(6):1151-1170
唐菊兴,宋扬,王勤,林彬,杨超,郭娜,方向,杨欢欢,王艺云,高轲,丁帅,张志,段吉琳,陈红旗,粟登逵,冯军,刘治博,韦少港,贺文,宋俊龙,李彦波,卫鲁杰.2016.西藏铁格隆南铜(金银)矿床地质特征及勘查模型---西藏首例千万吨级斑岩-浅成低温热液型矿床.地球学报,37(6):663-690
唐菊兴,王勤,杨欢欢,高昕,张泽斌,邹兵.2017.西藏斑岩-矽卡岩-浅成低温热液铜多金属矿成矿作用、勘查方向与资源潜力.地球学报,38(5):571-613
王德滋,周新民,徐夕生,姚玉鹏.1992.微粒花岗岩类包体的成因.桂林冶金地质学院学报,12(3):235-241
王德滋,谢磊.2008.岩浆混合作用:来自岩石包体的证据.高校地质学报,14(1):16-21
王勤,林彬,唐菊兴,宋扬,李彦波,侯俊富,李玉彬,卫鲁杰.2018.多龙矿集区色那东岩体年龄、成因与动力学背景.地球科学,43(4):1125-1141
王涛.2000.花岗岩混合成因研究及大陆动力学意义.岩石学报,16(2):161-168
王玉往,王京彬,龙灵利,邹滔,唐萍芝,王莉娟.2012.岩浆混合作用的类型、标志、机制、模式及其与成矿的关系---以新疆北部为例.岩石学报,28(8):2317-2330
韦少港,宋扬,唐菊兴,高轲,冯军,李彦波,侯淋.2016.西藏色那铜(金)矿床石英闪长玢岩年代学、地球化学与岩石成因.中国地质,43(6):1894-1912
韦少港,唐菊兴,宋扬,刘治博,王勤,林彬,贺文,冯军.2017a.西藏班公湖-怒江缝合带美日切错组中酸性火山岩锆石U-Pb年龄、Sr-Nd-Hf同位素、岩石成因及其构造意义.地质学报,91(1):132-150
韦少港,唐菊兴,宋扬,刘治博,王勤,林彬,王艺云,方向,杨欢欢,冯军.2017b.西藏改则多龙矿集区地堡那木岗矿床钾玄质二长花岗斑岩锆石LA-MC-ICP-MS U-Pb年龄、地球化学特征及其地质意义.地质论评,63(1):189-206
吴元保,郑永飞.2004.锆石成因矿物学研究及其对U-Pb年龄解释的制约.科学通报,49(16):1589-1604
肖庆辉,邓晋福,马大铨,洪大卫,莫宣学,卢欣祥,李志昌,汪雄武,马昌前,吴福元,罗照华,王涛.2002.花岗岩研究思维与方法.北京:地质出版社
许继峰,梅厚钧,于学元,白正华,牛贺才,陈繁荣,郑作平,王强.2001.准噶尔北缘晚古生代岛弧中与俯冲作用有关的adakite火山岩:消减板片部分熔融的产物.科学通报,46(8):684-688
于介江,侯雪刚,葛文春,张彦龙,柳佳成.2013.佳木斯地块东北缘早二叠世六连岩体的岩浆混合成因:岩相学、年代学和地球化学证据.岩石学报,29(9):2971-2986
张德全.1981.北京房山侵入体闪长质包体的特征及其成因探讨.地质论评,27(2):143-149
张旗,潘国强,李承东,金惟俊,贾秀勤.2007.花岗岩混合问题:与玄武岩对比的启示---关于花岗岩研究的思考之一.岩石学报,23(5):1141-1152
张志,方向,唐菊兴,王勤,杨超,王艺云,丁帅,杨欢欢.2017.西藏多龙矿集区尕尔勤斑岩铜矿床年代学及地球化学---兼论硅帽的识别与可能的浅成低温热液矿床.岩石学报,33(2):476-494
赵永久,袁超,周美夫,颜丹平,龙晓平,李继亮.2007.川西老君沟和孟通沟花岗岩的地球化学特征、成因机制及对松潘-甘孜地体基底性质的制约.岩石学报,23(5):995-1006
(1)秦克章,李光明,张旗,李金祥,缪宇,肖波,张天平,多吉,李金高,陆彦.2006.西藏浅成低温金-银矿的成矿条件与可能产出区分析---从斑岩-浅成低温铜金成矿系统的角度.见:中国科学院地质与地球物理研究所科技与成果转化处编.北京:中国科学院地质与地球物理研究所2006年论文摘要集,666-670
Barbarin B.2005.Mafic magmatic enclaves and mafic rocks associated with some granitoids of the central Sierra Nevada batholith,California:Nature,origin,and relations with the hosts.Lithos,80(1-4):155-177
Baxter S and Feely M.2002.Magma mixing and mingling textures in granitoids:Examples from the Galway granite,Connemara,Ireland.Mineralogy and Petrology,76(1-2):63-74
Belousova EA,Griffin WL,O’reilly SY and Fisher NI.2002.Igneous zircon:Trace element composition as an indicator of source rock type.Contributions to Mineralogy and Petrology,143:602-622
Bonin B.2004.Do coeval mafic and felsic magmas in post-collisional to within-plate regimes necessarily imply two contrasting,mantle and crustal,sources?A review.Lithos,78(1-2):1-24
Bonin B.2007.A-type granites and related rocks:Evolution of a concept,problems and prospects.Lithos,97(1-2):1-29
Boynton WV.1984.Geochemistry of the rare earth elements:Meteorite studies.In:Henderson P(ed.).Rare Earth Element Geochemistry.Amsterdam:Elsevier,63-114
Castro A.2013.Tonalite-granodiorite suites as cotectic systems:A review of experimental studies with applications to granitoid petrogenesis.Earth-Science Reviews,124:68-95
Champion DC and Bultitude RJ.2013.The geochemical and Sr-Nd isotopic characteristics of Paleozoic fractionated S-types granites of North Queensland:Implications for S-type granite petrogenesis.Lithos,162-163:37-56
Chappell BW and White AJR.1991.Restite enclaves and the restite model.In:Didier J and Barbarin B(eds.).Enclaves and Granite Petrology.Amsterdam:Elsevier,375-381
Chen B,Liu CQ and Tian W.2006.Magma-mixing between mantle-and crustal-derived melts in the process of Mesozoic magmatism,Taihangshan:Constraints from petrology and geochemistry.Earth Science Frontiers,13(2):140-147(in Chinese with English abstract)
Chen GJ,Sun FY,Li BL,Wang G,Qian Y,Xu QL and Liu GC.2014.Geochemistry and petrogenesis of Gouli mafic enclaves and their host rocks in eastern Kunlun.Journal of Jilin University(Earth Science Edition),44(3):892-904(in Chinese with English abstract)
Chen GC,Pei XZ,Li RB,Li ZC,Liu CJ,Chen YX,Xu T and Zhang YM.2016.Genesis of magma mixing and mingling of Xiangjiananshan granite batholith in the eastern section of East Kunlun orogen:Evidence from mafic microgranular enclaves(MMEs).Earth Science Frontiers,23(4):226-240(in Chinese with English abstract)
Didier J.1973.Granites and Their Enclaves:The Bearing of Enclaves on the Origin of Granites.Amsterdam:Elsevier,1-393
Ding S,Tang JX,Zheng WB,Yang C,Zhang Z,Wang Q and Wang YY.2017.Geochronology and geochemistry of Naruo porphyry Cu(Au)deposit in Duolong ore-concentrated area,Tibet,and their geological significance.Earth Science,42(1):1-23(in Chinese with English abstract)
Dong GC,Mo XX,Zhao ZD,Zhu DC,Wang LL,Chen T and Li B.2006.Magma mixing in middle part of Gangdise magma belt:Evidences from granitoid complex.Acta Petrologica Sinica,22(4):835-844(in Chinese with English abstract)
Du DD,Qu XM,Wang GH,Xin HB and Liu ZB.2011.Bidirectional subduction of the Middle Tethys oceanic basin in the west segment of Bangonghu-Nujiang suture,Tibet:Evidence from zircon U-Pb LAICPMS dating and petrogeochemistry of arc granites.Acta Petrologica Sinica,27(7):1993-2002(in Chinese with English abstract)
Eichelberger JC.1980.Vesiculation of mafic magma during replenishment of silicic magma reservoirs.Nature,288(5790):446-450
Feeley TC,Wilson LF and Underwood SJ.2008.Distribution and compositions of magmatic inclusions in the Mount Helen dome,Lassen Volcanic Center,California:Insights into magma chamber processes.Lithos,106(1-2):173-189
Frost TP and Mahood GA.1987.Field,chemical,and physical constraints on mafic-felsic magma interaction in the Lamarck granodiorite,Sierra Nevada,California.Geological Society of America Bulletin,99(2):272-291
Fu Q,Ge WS,Wen CS,Cai KQ,Li SF,Zhang ZW and Li XF.2011.Geochemistry and genesis of Michang granites and their dark microgranular enclaves in Guangxi.Acta Geoscientica Sinica,32(3):293-303(in Chinese with English abstract)
Gu FH,Zhang YM,Liu RP,Zheng L and Sun X.2015.Magma mixing and mingling of the Shadegai granite in Inner Mongolia:Evidence from petrography,mineral chemistry and geochronology.Acta Petrologica Sinica,31(5):1374-1390(in Chinese with English abstract)
Hao BW.2012.Discovery,genesis and tectonic significance of the LatePaleozoic miarolitic K-feldspar granite in southern Xianghuangqi,Inner Mongolia.Journal of Jilin University(Earth Science Edition),42(2):269-284(in Chinese with English abstract)
Huang QS,Shi RD,Ding BH,Liu DL,Zhang XR,Fan SQ and Zhi XC.2012.Re-Os isotopic evidence of MOR-type ophiolite from the Bangong Co for the opening of Bangong-Nujiang Tethys Ocean.Acta Petrologica et Mineralogica,31(4):465-478(in Chinese with English abstract)
Huppert EH and Sparks RSJ.1988.The generation of granitic magmas by intrusion of basalt into continental crust.Journal of Petrology,29(3):599-624
Jin XC and Yu KP.2003.Subduction factory and subduction recycling of continental material.Advance in Earth Sciences,18(5):737-744(in Chinese with English abstract)
Jochum KP,Mc Donough WF,Palme H and Spettel B.1989.Compositional constraints on the continental lithospheric mantle from trace elements in spinel peridotite xenoliths.Nature,340(6234):548-550
Jung S and Pfnder JA.2007.Source composition and melting temperatures of orogenic granitoids:Constraints from CaO/Na2O,Al2O3/Ti O2and accessory mineral saturation thermometry.European Journal of Mineralogy,19(6):859-870
Kang L,Li YJ,Zhang B,Zhang HW and Wang JN.2009.Petrographic evidence for magma mixing of Xiaerpu granite in West Junggar,Xinjiang.Acta Petrologica et Mineralogica,28(5):423-432(in Chinese with English abstract)
Kapp P,Yin A,Harrison TM and Lin D.2005.Cretaceous-Tertiary shortening,basin development,and volcanism in central Tibet.Geological Society of America Bulletin,117(7-8):865-878
Kumar S and Rino V.2006.Mineralogy and geochemistry of microgranular enclaves in Palaeoproterozoic Malanjkhand granitoids,central India:Evidence of magma mixing,mingling,and chemical equilibration.Contributions to Mineralogy and Petrology,152(5):591-609
Kumar S and Pieru T.2010.Petrography and major elements geochemistry of microgranular enclaves and Neoproterozoic granitoids of South Khasi,Meghalaya:Evidence of magma mixing and alkali diffusion.Journal of the Geological Society of India,76(4):345-360
Lei CY,Li ZJ,Zhang Z,Hu ZH,Wang HX and Song JL.2012.Geochemical characteristics and geodynamic significance of the granites in the Ga’erqiong Cu-Au deposit,Tibet.Acta Geoscientica Sinica,33(4):601-612(in Chinese with English abstract)
Lei CY,Wu JL,Yin XK,Liu W,Wang B,Li W,Yuan HY,Zhang W,Yin T and Pei YL.2018.New discovery of the diorite porphyry dyke in the Shamuluo formation in western segment of the BangongcoNujiang suture zone and its geological significance.Bulletin of Mineralogy,Petrology and Geochemistry,37(2):250-259(in Chinese with English abstract)
Lei CY,Wu JL,Yin XK,Liu W,Wang B,Li W,Yuan HY,Zhang W,Yin T and Pei YL.2019.Petrogenesis of intermediate-acid intrusive rocks in Awengcuo area in the west segment of the BangongcoNujiang Suture,Tibet,and its instructions to the regional tectonic evolution.Geotectonica et Metallogenia,43(1):168-185(in Chinese with English abstract)
Lei M,Chen JL,Xu JF and Zeng YC.2015.Geochemistry of early Late Cretaceous Gaerqiong high-Mg#diorite porphyry in midnorthern Lhasa terrane:Partial melting of delaminated lower continental crust?Geological Bulletin of China,34(2-3):337-346(in Chinese with English abstract)
Li CN.1999.Discovery for Precambrian magmatic mixed zone from northeastern Jiangxi Province and their geological significance.Earth Science Frontiers,6(4):331-337(in Chinese with English abstract)
Li FQ,Liu ZB,Tang JX,Song Y,Gao K,Li HF,Zhao ZQ and Teng L.2018.Petrogenesis of granite porphyry in mariaicuo area,Shuanghu County,Tibet,and constraints on the evolution in the middle section of Bangonghu-Nujiang suture zone.Earth Science,43(4):1051-1069(in Chinese with English abstract)
Li GM,Zhang XN,Qin KZ,Sun XG,Zhao JX,Yin XB,Li JX and Yuan HS.2015.The telescoped porphyry-high sulfidation epithermal Cu(-Au)mineralization of Rongna deposit in Duolong ore cluster at the southern margin of Qiangtang Terane,Central Tibet:Integrated evidence from geology,hydrothermal alteration and sulfide assemblages.Acta Petrologica Sinica,31(8):2307-2324(in Chinese with English abstract)
Li HL,Gao C,Li ZH,Zhang Z,Peng ZM and Guan JL.2016.Age and tectonic significance of Jingzhushan Formation in Bangong Lake area,Tibet.Geotectonica et Metallogenia,40(4):663-673(in Chinese with English abstract)
Li JX,Qin KZ and Li GM.2006.Basic characteristics of gold-rich porphyry copper deposits and their ore sources and evolving processes of high oxidation magma and ore-forming fluid.Acta Petrologica Sinica,22(3):678-688(in Chinese with English abstract)
Li JX.2008.Geochronology,petrology and metallogeneses of high oxidized magma-hydrothermal fluid of Duobuza gold-rich porphyry copper deposit in Bangonghu belt,Northern Tibet.Ph.D.Dissertation.Beijing:Institute of Geology and Geophysics,Chinese Academy of Sciences 1-224(in Chinese with English summary)
Li JX,Qin KZ,Li GM,Xiao B,Zhao JX,Cao MJ and Chen L.2013.Petrogenesis of ore-bearing porphyries from the Duolong porphyry CuAu deposit,central Tibet:Evidence from U-Pb geochronology,petrochemistry and Sr-Nd-Hf-O isotope characteristics.Lithos,160-161:216-227
Li XH,Zhou HW,Liu Y,Lee CY,Chen ZH,Yu JS and Gui XT.2000.Mesozoic shoshonitic intrusives in the Yangchun Basin,western Guangdong,and their tectonic significance:Ⅰ.Petrology and isotope geochronology.Geochimica,29(6):513-520(in Chinese with English abstract)
Lin B,Chen YC,Tang JX,Wang Q,Song Y,Yang C,Wang WL,He W and Zhang LJ.2017a.40Ar/39Ar and Rb-Sr ages of the Tiegelongnan porphyry Cu-(Au)deposit in the Bangong Co-Nujiang metallogenic belt of Tibet,China:Implication for generation of super-large deposit.Acta Geologica Sinica,91(2):602-616
Lin B,Tang JX,Chen YC,Song Y,Hall G,Wang Q,Yang C,Fang X,Duan JL,Yang HH,Liu ZB,Wang YY and Feng J.2017b.Geochronology and genesis of the Tiegelongnan porphyry Cu(Au)deposit in Tibet:Evidence from U-Pb,Re-Os dating and Hf,S,and H-O isotopes.Resource Geology,67(1):1-21
Lin B,Tang JX,Song Y,Wang Q,Cao HW,Baker M,Zhang LJ and Li YB.2017.Petrogeochemistry and SHRIMP dating of Ga’erqin pillow basalt in Duolong,Northern Tibet.Acta Geoscientica Sinica,38(5):702-710(in Chinese with English abstract)
Lin B,Tang JX,Chen YC,Baker M,Song Y,Yang HH,Wang Q,He W and Liu ZB.2019.Geology and geochronology of Naruo large porphyry-breccia Cu deposit in the Duolong district,Tibet.Gondwana Research,66:168-182
Liu YS,Hu ZC,Gao S,Günther D,Xu J,Gao CG and Chen HH.2008.In situ analysis of major and trace elements of anhydrous minerals by LA-ICP-MS without applying an internal standard.Chemical Geology,257(1-2):34-43
Liu YS,Hu ZC,Zong KQ,Gao CG,Gao S,Xu J and Chen HH.2010.Reappraisement and refinement of zircon U-Pb isotope and trace element analyses by LA-ICP-MS.Chinese Science Bulletin,55(15):1535-1546
Ma CQ,Yang KG,Tang ZH and Li ZT.1994.Magma-Dynamics of Granitoids Theory,Method and A Case Study of the Eastern Hubei Granitoids.Wuhan:China University of Geosciences Press(in Chinese)
Ma LT,Zhang ZC,Dong SY,Zhang S,Zhang DY and Huang H.2010.Geology and geochemistry of the Yingmailai granitic intrusion in the Southern Tianshan and its implications.Earth Science(Journal of China University of Geosciences),35(6):908-920(in Chinese with English abstract)
Maas R,Nicholls IA and Legg C.1997.Igneous and metamorphic enclaves in the S-type Deddick granodiorite,Lachlan Fold Belt,SEAustralia:Petrographic,geochemical and Nd-Sr isotopic evidence for crustal melting and magma mixing.Journal of Petrology,38(7):815-841
Mc Donough WF,Sun SS,Ringwood AE,Jagoutz E and Hofmann AW.1992.Potassium,rubidium,and cesium in the Earth and Moon and the evolution of the mantle of the Earth.Geochimica et Cosmochimica Acta,56(3):1001-1012
Mo XX.2011.Magma and magmatic/igneous rocks:A lithoprobe into the deep earth and records of the earth’s evolution.Chinese Journal of Nature,33(5):255-259(in Chinese with English abstract)
Montel JM and Vielzeuf D.1997.Partial melting of metagreywackes,PartⅡ.Compositions of minerals and melts.Contributions to Mineralogy and Petrology,128(2-3):176-196
Noyes HJ,Frey FA and Wones DR.1983.A tale of two plutons:Geochemical evidence bearing on the origin and differentiation of the Red Lake and Eagle Peak plutons,Central Sierra Nevada,California.The Journal of Geology,91(5):487-509
Paterson SR,Pignotta GS and Vernon RH.2004.The significance of microgranitoid enclave shapes and orientations.Journal of Structural Geology,26(8):1465-1481
Pearce JA.1996.Sources and settings of granitic rocks.Episodes,19(4):120-125
Perugini D,Poli G,Christofides G and Eleftheriadis G.2003.Magma mixing in the Sithonia plutonic complex,Greece:Evidence from mafic microgranular enclaves.Mineralogy and Petrology,78(3-4):173-200
Qi YQ,Hu RZ,Liu S and Tian JJ.2008.Review on magma mixing and mingling.Bulletin of Mineralogy,Petrology and Geochemistry,27(4):409-416(in Chinese with English abstract)
Qiangba ZX,Xie YW,Wu YW,Xie CM,Li QL and Qiu JQ.2009.Zircon SIMS U-Pb dating and its significance of cumulate gabbro from Dengqen ophiolite,eastern Tibet,China.Geological Bulletin of China,28(9):1253-1258(in Chinese with English abstract)
Qiangba ZX,Wu H,Gesang WD,Ciren OZ,Basang DZ,Qiong D and Niu DW.2016.Early Cretaceous magmatism in Dongqiao,Tibet:Implications for the evolution of the Bangong-Nujiang Ocean and crustal growth in a continent-continent collision zone.Geological Bulletin of China,35(5):648-666(in Chinese with English abstract)
Qiu JS,Wang RQ,Zhao JL and Yu SB.2015.Petrogenesis of the Early Jurassic gabbro-granite complex in the middle segment of the Gangdese belt and its implications for tectonic evolution of NeoTethys:A case study of the Dongga pluton in Xi’gaze.Acta Petrologica Sinica,31(22):3569-3580(in Chinese with English abstract)
Qu XM,Wang RJ,Xin HB,Zhao YY and Fan XT.2009.Geochronology and geochemistry of igneous rocks related to the subduction of the Tethys oceanic plate along the Bangong Lake arc zone,the western Tibetan Plateau.Geochimica,38(6):523-535(in Chinese with English abstract)
Ren JS,Niu BG and Liu ZG.1999.Soft collision,superposition orogeny and polycyclic suturing.Earth Science Frontiers,6(3):85-93(in Chinese with English abstract)
Rickwood PC.1989.Boundary lines within petrologic diagrams which use oxides of major and minor elements.Lithos,22(4):247-263
Rudnick RL and Gao S.2003.Composition of the continental crust.In:Rudniek RL(ed.).Treatise on Geochemistry.Amsterdam:Elsevier,1-64
Rushmer T.1991.Partial melting of two amphibolites:Contrasting experimental results under fluid-absent conditions.Contributions to Mineralogy and Petrology,107(1):41-59
Shamberger PJ and Garcia MO.2007.Geochemical modeling of magma mixing and magma reservoir volumes during early episodes of Kīlauea Volcano’s Pu‘u‘‘ōeruption.Bulletin of Volcanology,69(4):345-352
Shellnutt JG,Jahn BM and Dostal J.2010.Elemental and Sr-Nd isotope geochemistry of microgranular enclaves from peralkaline A-type granitic plutons of the Emeishan large igneous province,SW China.Lithos,119(1):34-46
Shi RD,Griffin WL,O’Reilly SY,Huang QS,Zhang XR,Liu DL,Zhi XC,Xia QX and Ding L.2012.Melt/mantle mixing produces podiform chromite deposits in ophiolites:Implications of Re-Os systematics in the Dongqiao Neo-Tethyan ophiolite,northern Tibet.Gondwana Research,21(1):194-206
Song B,Zhang YH,Wan YS and Jian P.2002.Mount making and procedure of the SHRIMP dating.Geological Review,48(Suppl.):26-30(in Chinese with English abstract)
Song Y,Qu XM,Xin HB,Wang ZY and Du DD.2013.The crustal carbon cycling in the Late Cretaceous extension of Bangong Lake arc zone in the Xizang(Tibetan)Plateau.Geological Review,59(2):225-233(in Chinese with English abstract)
Song Y,Yang HH,Lin B,Liu ZB,Wang Q,Gao K,Yang C and Fang X.2017.The preservation system of epithermal deposits in South Qiangtang terrane of central Tibetan Plateau and its significance:Acase study of the Tiegelongnan superlarge deposit.Acta Geoscientica Sinica,38(5):659-669(in Chinese with English abstract)
Song Y,Yang C,Wei SG,Yang HH,Fang X and Lu HT.2018.Tectonic control,reconstruction and preservation of the Tiegelongnan porphyry and epithermal overprinting Cu(Au)deposit,Central Tibet,China.Minerals,8(9):398
Spring L,Bussy F,Vannay J C,Huon S and Cosca MA.1993.Early Permian granitic dykes of alkaline affinity in the Indian High Himalaya of upper Lahul and SE Zanskar:Geochemical characterization and geotectonic implications.Geological Society,London,Special Publications,74(1):251-264
Stampfli GM and Borel GD.2002.A plate tectonic model for the Paleozoic and Mesozoic constrained by dynamic plate boundaries and restored synthetic oceanic isochrons.Earth and Planetary Science Letters,196(1-2):17-33
Tang JX,Sun XG,Ding S,Wang Q,Wang YY,Yang C,Chen HQ,Li YB,Li YB,Wei LJ,Zhang Z,Song JL,Yang HH,Duan JL,Gao K,Fang X and Tan JY.2014a.Discovery of the epithermal deposit of Cu(Au-Ag)in the Duolong ore concentrating area,Tibet.Acta Geoscientica Sinica,35(1):6-10(in Chinese with English abstract)
Tang JX,Wang Q,Yang C,Ding S,Lang XH,Liu HF,Huang Y,Zheng WB,Wang LQ,Gao YM,Feng J,Duan JL,Song Y,Wang YY,Lin B,Fang X,Zhang Z and Yang HH.2014b.Two porphyryepithermal deposit metallogenic subseries in Tibetan Plateau:Practice of“absence prospecting”deposit metallogenic series.Mineral Deposits,33(6):1151-1170(in Chinese with English abstract)
Tang JX,Song Y,Wang Q,Lin B,Yang C,Guo N,Fang X,Yang HH,Wang YY,Gao K,Ding S,Zhang Z,Duan JL,Chen HQ,Su DK,Feng J,Liu ZB,Wei SG,He W,Song JL,Li YB and Wei LJ.2016.Geological characteristics and exploration model of the Tiegelongnan Cu(Au-Ag)deposit:The first ten million tons metal resources of a porphyry-epithermal deposit in Tibet.Acta Geoscientica Sinica,37(6):663-690(in Chinese with English abstract)
Tang JX,Wang Q,Yang HH,Gao X,Zhang ZB and Zou B.2017.Mineralization,exploration and resource potential of porphyry-skarnepithermal copper polymetallic deposits in Tibet.Acta Geoscientica Sinica,38(5):571-613(in Chinese with English abstract)
Troll VR and Schmincke HU.2002.Magma mixing and crustal recycling recorded in ternary feldspar from compositionally zoned peralkaline ignimbrite‘A’,Gran Canaria,Canary Islands.Journal of Petrology,43(2):243-270
Vernon RH.1983.Restite,xenoliths and microgranitoid enclaves in granites.Journal and Proceedings,Royal Society of New South Wales,116(3):77-103
Vernon RH.2014.Microstructures of microgranitoid enclaves and the origin of S-type granitoids.Australian Journal of Earth Sciences,61(2):227-239
Wang BD,Wang LQ,Chung SL,Chen JL,Yin FG,Liu H,Li XB and Chen LK.2016.Evolution of the Bangong-Nujiang Tethyan Ocean:Insights from the geochronology and geochemistry of mafic rocks within ophiolites.Lithos,245:18-33
Wang DZ,Zhou XM,Xu XS and Yao YP.1992.On geneses of microgranitoid enclaves.Journal of Guilin College of Geology,12(3):235-241(in Chinese)
Wang DZ and Xie L.2008.Magma mingling:Evidence from enclaves.Geological Journal of China Universities,14(1):16-21(in Chinese with English abstract)
Wang Q,Lin B,Tang JX,Song Y,Li YB,Hou JF,Li YB and Wei LJ.2018.Diagenesis,lithogenesis and geodynamic setting of intrusions in Senadong area,Duolong district,Tibet.Earth Science,43(4):1125-1141(in Chinese with English abstract)
Wang T.2000.Origin of hybrid granitoids and the implications for continental dynamics.Acta Petrologica Sinica,16(2):161-168(in Chinese with English abstract)
Wang YW,Wang JB,Long LL,Zou T,Tang PZ and Wang LJ.2012.Type,indicator,mechanism,model and relationship with mineralization of magma mixing:A case study in North Xinjiang.Acta Petrologica Sinica,28(8):2317-2330(in Chinese with English abstract)
Wei SG,Song Y,Tang JX,Gao K,Feng J,Li YB and Hou L.2016.Geochronology,geochemistry and petrogenesis of quartz diorite porphyrite from the Sena copper(gold)deposit,Tibet.Geology in China,43(6):1894-1912(in Chinese with English abstract)
Wei SG,Tang JX,Song Y,Liu ZB,Wang Q,Lin B,He W and Feng J.2017a.Petrogenesis,zircon U-Pb geochronology and Sr-Nd-Hf isotopes of the intermediate-felsic volcanic rocks from the Duolong deposit in the Bangonghu-Nujiang suture zone,Tibet,and its tectonic significance.Acta Geologica Sinica,91(1):132-150(in Chinese with English abstract)
Wei SG,Tang JX,Song Y,Liu ZB,Wang Q,Lin B,Wang YY,Fang X,Yang HH and Feng J.2017b.Zircons LA-MC-ICP-MS U-Pb ages,petrochemical,petrological and its significance of the Potassic monzonitic granite porphyry from the Duolong ore concentrated district,Gaize County,Xizang(Tibet).Geological Review,63(1):189-206(in Chinese with English abstract)
Winther KT.1996.An experimentally based model for the origin of tonalitic and trondhjemitic melts.Chemical Geology,127(1-3):43-59
Wu YB and Zheng YF.2004.Genesis of zircon and its constraints on interpretation of U-Pb age.Chinese Science Bulletin,49(15):1554-1569
Xiao QH,Deng JF,Ma DQ,Hong DW,Mo XX,Lu XX,Li ZC,Wang XW,Ma CQ,Wu FY,Luo ZH and Wang T.2002.The Ways of Investigation on Granitoids.Beijing:Geological Publishing House(in Chinese)
Xu JF,Mei HJ,Yu XY,Bai ZH,Niu HC,Chen FR,Zheng ZP and Wang Q.2001.Adakites related to subduction in the northern margin of Junggar arc for the Late Paleozoic:Products of slab melting.Chinese Science Bulletin,46:684-688(in Chinese)
Yu JJ,Hou XG,Ge WC,Zhang YL and Liu JC.2013.Magma mixing genesis of the Early Permian Liulian pluton at the northeastern margin of the Jiamusi massif in NE China:Evidences from petrography,geochronology and geochemistry.Acta Petrologica Sinica,29(9):2971-2986(in Chinese with English abstract)
Zhang C,Liu CZ,Wu FY,Zhang LL and Ji WQ.2016.Geochemistry and geochronology of mafic rocks from the Luobusa ophiolite,South Tibet.Lithos,245:93-108
Zhang DQ.1981.The characteristics and origin of the dioritic inclusions in the Fangshan intrusion,Beijing.Geological Review,27(2):143-149(in Chinese with English abstract)
Zhang Q,Pan GQ,Li CD,Jin WJ and Jia XQ.2007.Granitic magma mixing versus basaltic magma mixing:New viewpoints on granitic magma mixing process:Some crucial questions on granite study(1).Acta Petrologica Sinica,23(5):1141-1152(in Chinese with English abstract)
Zhang Z,Fang X,Tang JX,Wang Q,Yang C,Wang YY,Ding S and Yang HH.2017.Chronology,geochemical characteristics of the Gaerqin porphyry copper deposit in the Duolong ore concentration area in Tibet and discussion about the identification of the lithoscaps and the possible epithermal deposit.Acta Petrologica Sinica,33(2):476-494(in Chinese with English abstract)
Zhao YJ,Yuan C,Zhou MF,Yan DP,Long XP and Li JG.2007.Geochemistry and petrogenesis of Laojungou and Mengtonggou granites in western Sichuan,China:Constraints on the nature of Songpan-Ganzi basement.Acta Petrologica Sinica,23(5):995-1006(in Chinese with English abstract)
Zhou WG,Xie HS,Liu YG,Zheng XG,Zhao ZD and Zhou H.2005.Dehydration melting of solid amphibolite at 2.0GPa:Effects of time and temperature.Science in China(Series D),48(8):1120-1133
Zhu DC,Mo XX,Zhao ZD,Niu Y,Wang LQ,Chu QH,Pan GT,Xu JF and Zhou CY.2010.Presence of Permian extension-and arc-type magmatism in southern Tibet:Paleogeographic implications.Geological Society of America Bulletin,122(7-8):979-993
陈斌,刘超群,田伟.2006.太行山中生代岩浆作用过程中的壳幔岩浆混合作用:岩石学和地球化学证据.地学前缘,13(2):140-147
陈广俊,孙丰月,李碧乐,王冠,钱烨,许庆林,刘国才.2014.东昆仑沟里地区暗色包体及其寄主岩石地球化学特征及成因.吉林大学学报(地球科学版),44(3):892-904
陈国超,裴先治,李瑞保,李佐臣,刘成军,陈有炘,徐通,张永明.2016.东昆仑东段香加南山花岗岩基的岩浆混合成因:来自镁铁质微粒包体的证据.地学前缘,23(4):226-240
丁帅,唐菊兴,郑文宝,杨超,张志,王勤,王艺云.2017.西藏拿若斑岩型铜(金)矿含矿岩体年代学、地球化学及地质意义.地球科学,42(1):1-23
董国臣,莫宣学,赵志丹,朱弟成,王亮亮,陈涛,李冰.2006.冈底斯岩浆带中段岩浆混合作用:来自花岗杂岩的证据.岩石学报,22(4):835-844
杜德道,曲晓明,王根厚,辛洪波,刘治博.2011.西藏班公湖-怒江缝合带西段中特提斯洋盆的双向俯冲:来自岛弧型花岗岩锆石U-Pb年龄和元素地球化学的证据.岩石学报,27(7):1993-2002
付强,葛文胜,温长顺,蔡克勤,李世富,张志伟,李小飞.2011.广西米场花岗岩及其暗色微粒包体的地球化学特征和成因分析.地球学报,32(3):293-303
顾枫华,章永梅,刘瑞萍,郑硌,孙玄.2015.内蒙古沙德盖花岗岩岩浆混合作用:岩相学、矿物化学和年代学证据.岩石学报,31(5):1374-1390
郝百武.2012.内蒙古镶黄旗南晚古生代晶洞钾长花岗岩杂岩的发现、岩石成因及其构造意义.吉林大学学报(地球科学版),42(2):269-284
黄启帅,史仁灯,丁炳华,刘德亮,张晓冉,樊帅权,支霞臣.2012.班公湖MOR型蛇绿岩Re-Os同位素特征对班公湖-怒江特提斯洋裂解时间的制约.岩石矿物学杂志,31(4):465-478
金性春,于开平.2003.俯冲工厂和大陆物质的俯冲再循环研究.地球科学进展,18(5):737-744
康磊,李永军,张兵,张洪伟,王军年.2009.新疆西准噶尔夏尔莆岩体岩浆混合的岩相学证据.岩石矿物学杂志,28(5):423-432
雷传扬,李志军,张志,胡正华,王红星,宋俊龙.2012.西藏尕尔穷铜金矿床花岗岩类的地球化学特征及其地球动力学意义.地球学报,33(4):601-612
雷传扬,吴建亮,尹显科,刘文,王波,李威,袁华云,张伟,尹滔,裴亚伦.2018.班公湖-怒江缝合带西段沙木罗组地层中闪长玢岩脉的发现及其地质意义.矿物岩石地球化学通报,37(2):250-259
雷传扬,吴建亮,尹显科,刘文,王波,李威,袁华云,张伟,尹滔,裴亚伦.2019.班公湖-怒江缝合带西段阿翁错地区中酸性侵入岩的成因及其对区域构造演化的指示.大地构造与成矿学,43(1):168-185
雷鸣,陈建林,许继峰,曾云川.2015.拉萨地体中北部尕尔穷晚白垩世早期高镁闪长玢岩地球化学特征指示:加厚下地壳的拆沉?地质通报,34(2-3):337-346
李昌年.1999.赣东北前寒武纪岩浆混合作用岩带的发现及其地质意义.地学前缘,6(4):331-337
李发桥,刘治博,唐菊兴,宋扬,高轲,李海峰,赵志强,滕磊.2018.西藏玛日埃错地区花岗斑岩岩石成因及其对班公湖-怒江缝合带中段演化的制约.地球科学,43(4):1051-1069
李光明,张夏楠,秦克章,孙兴国,赵俊兴,印贤波,李金祥,袁华山.2015.羌塘南缘多龙矿集区荣那斑岩-高硫型浅成低温热液Cu-(Au)套合成矿:综合地质、热液蚀变及金属矿物组合证据.岩石学报,31(8):2307-2324
李华亮,高成,李正汉,张璋,彭智敏,关俊雷.2016.西藏班公湖地区竟柱山组时代及其构造意义.大地构造与成矿学,40(4):663-673
李金祥,秦克章,李光明.2006.富金斑岩型铜矿床的基本特征、成矿物质来源与成矿高氧化岩浆-流体演化.岩石学报,22(3):678-688
李金祥.2008.班公湖带多不杂超大型富金斑岩铜矿床的成岩成矿年代学、岩石学及高氧化岩浆-流体-成矿作用.博士学位论文.北京:中国科学院地质与地球物理研究所,1-224
李献华,周汉文,刘颖,李寄嵎,陈正宏,于津生,桂训唐.2000.粤西阳春中生代钾玄质侵入岩及其构造意义:Ⅰ.岩石学和同位素地质年代学.地球化学,29(6):513-520
林彬,唐菊兴,宋扬,王勤,曹华文,Baker M,张乐骏,李玉彬.2017.藏北多龙矿集区尕尔勤枕状玄武岩地球化学及SHRIMP测年.地球学报,38(5):702-710
马昌前,杨坤光,唐仲华,李增田.1994.花岗岩类岩浆动力学:理论方法及鄂东花岗岩类例析.武汉:中国地质大学出版社
马乐天,张招崇,董书云,张舒,张东阳,黄河.2010.南天山英买来花岗岩的地质、地球化学特征及其地质意义.地球科学-中国地质大学学报,35(6):908-920
莫宣学.2011.岩浆与岩浆岩:地球深部“探针”与演化记录.自然杂志,33(5):255-259
齐有强,胡瑞忠,刘燊,田建吉.2008.岩浆混合作用研究综述.矿物岩石地球化学通报,27(4):409-416
强巴扎西,谢尧武,吴彦旺,解超明,李秋立,邱军强.2009.藏东丁青蛇绿岩中堆晶辉长岩锆石SIMS U-Pb定年及其意义.地质通报,28(9):1253-1258
强巴扎西,吴浩,格桑旺堆,次仁欧珠,巴桑顿珠,琼达,女达娃.2016.班公湖-怒江缝合带中段东巧地区早白垩世岩浆作用---对大洋演化和地壳增厚的指示.地质通报,35(5):648-666
邱检生,王睿强,赵姣龙,喻思斌.2015.冈底斯中段早侏罗世辉长岩-花岗岩杂岩体成因及其对新特提斯构造演化的启示:以日喀则东嘎岩体为例.岩石学报,31(12):3569-3580
曲晓明,王瑞江,辛洪波,赵元艺,樊兴涛.2009.西藏西部与班公湖特提斯洋盆俯冲相关的火成岩年代学和地球化学.地球化学,38(6):523-525
任纪舜,牛宝贵,刘志刚.1999.软碰撞、叠覆造山和多旋回缝合作用.地学前缘,6(3):85-93
宋彪,张玉海,万渝生,简平.2002.锆石SHRIMP样品靶制作、年龄测定及有关现象讨论.地质论评,48(增):26-30
宋扬,曲晓明,辛洪波,王志云,杜德道.2013.西藏班公湖岛弧带晚白垩世地壳伸展期间碳的壳内循环.地质论评,59(2):225-233
宋扬,杨欢欢,林彬,刘治博,王勤,高轲,杨超,方向.2017.青藏高原羌塘地体南缘浅成低温热液成矿系统的保存机制及其重要意义---以铁格隆南超大型矿床为例.地球学报,38(5):659-669
唐菊兴,孙兴国,丁帅,王勤,王艺云,杨超,陈红旗,李彦波,李玉彬,卫鲁杰,张志,宋俊龙,杨欢欢,段吉琳,高轲,方向,谭江云.2014a.西藏多龙矿集区发现浅成低温热液型铜(金银)矿床.地球学报,35(1):6-10
唐菊兴,王勤,杨超,丁帅,郎兴海,刘鸿飞,黄勇,郑文宝,王立强,高一鸣,冯军,段吉琳,宋杨,王艺云,林彬,方向,张志,杨欢欢.2014b.青藏高原两个斑岩-浅成低温热液矿床成矿亚系列及其“缺位找矿”之实践.矿床地质,33(6):1151-1170
唐菊兴,宋扬,王勤,林彬,杨超,郭娜,方向,杨欢欢,王艺云,高轲,丁帅,张志,段吉琳,陈红旗,粟登逵,冯军,刘治博,韦少港,贺文,宋俊龙,李彦波,卫鲁杰.2016.西藏铁格隆南铜(金银)矿床地质特征及勘查模型---西藏首例千万吨级斑岩-浅成低温热液型矿床.地球学报,37(6):663-690
唐菊兴,王勤,杨欢欢,高昕,张泽斌,邹兵.2017.西藏斑岩-矽卡岩-浅成低温热液铜多金属矿成矿作用、勘查方向与资源潜力.地球学报,38(5):571-613
王德滋,周新民,徐夕生,姚玉鹏.1992.微粒花岗岩类包体的成因.桂林冶金地质学院学报,12(3):235-241
王德滋,谢磊.2008.岩浆混合作用:来自岩石包体的证据.高校地质学报,14(1):16-21
王勤,林彬,唐菊兴,宋扬,李彦波,侯俊富,李玉彬,卫鲁杰.2018.多龙矿集区色那东岩体年龄、成因与动力学背景.地球科学,43(4):1125-1141
王涛.2000.花岗岩混合成因研究及大陆动力学意义.岩石学报,16(2):161-168
王玉往,王京彬,龙灵利,邹滔,唐萍芝,王莉娟.2012.岩浆混合作用的类型、标志、机制、模式及其与成矿的关系---以新疆北部为例.岩石学报,28(8):2317-2330
韦少港,宋扬,唐菊兴,高轲,冯军,李彦波,侯淋.2016.西藏色那铜(金)矿床石英闪长玢岩年代学、地球化学与岩石成因.中国地质,43(6):1894-1912
韦少港,唐菊兴,宋扬,刘治博,王勤,林彬,贺文,冯军.2017a.西藏班公湖-怒江缝合带美日切错组中酸性火山岩锆石U-Pb年龄、Sr-Nd-Hf同位素、岩石成因及其构造意义.地质学报,91(1):132-150
韦少港,唐菊兴,宋扬,刘治博,王勤,林彬,王艺云,方向,杨欢欢,冯军.2017b.西藏改则多龙矿集区地堡那木岗矿床钾玄质二长花岗斑岩锆石LA-MC-ICP-MS U-Pb年龄、地球化学特征及其地质意义.地质论评,63(1):189-206
吴元保,郑永飞.2004.锆石成因矿物学研究及其对U-Pb年龄解释的制约.科学通报,49(16):1589-1604
肖庆辉,邓晋福,马大铨,洪大卫,莫宣学,卢欣祥,李志昌,汪雄武,马昌前,吴福元,罗照华,王涛.2002.花岗岩研究思维与方法.北京:地质出版社
许继峰,梅厚钧,于学元,白正华,牛贺才,陈繁荣,郑作平,王强.2001.准噶尔北缘晚古生代岛弧中与俯冲作用有关的adakite火山岩:消减板片部分熔融的产物.科学通报,46(8):684-688
于介江,侯雪刚,葛文春,张彦龙,柳佳成.2013.佳木斯地块东北缘早二叠世六连岩体的岩浆混合成因:岩相学、年代学和地球化学证据.岩石学报,29(9):2971-2986
张德全.1981.北京房山侵入体闪长质包体的特征及其成因探讨.地质论评,27(2):143-149
张旗,潘国强,李承东,金惟俊,贾秀勤.2007.花岗岩混合问题:与玄武岩对比的启示---关于花岗岩研究的思考之一.岩石学报,23(5):1141-1152
张志,方向,唐菊兴,王勤,杨超,王艺云,丁帅,杨欢欢.2017.西藏多龙矿集区尕尔勤斑岩铜矿床年代学及地球化学---兼论硅帽的识别与可能的浅成低温热液矿床.岩石学报,33(2):476-494
赵永久,袁超,周美夫,颜丹平,龙晓平,李继亮.2007.川西老君沟和孟通沟花岗岩的地球化学特征、成因机制及对松潘-甘孜地体基底性质的制约.岩石学报,23(5):995-1006
(1)秦克章,李光明,张旗,李金祥,缪宇,肖波,张天平,多吉,李金高,陆彦.2006.西藏浅成低温金-银矿的成矿条件与可能产出区分析---从斑岩-浅成低温铜金成矿系统的角度.见:中国科学院地质与地球物理研究所科技与成果转化处编.北京:中国科学院地质与地球物理研究所2006年论文摘要集,666-670
© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号 地址：北京市海淀区学院路29号 邮编：100083 电话：办公室：(+86 10)66554848；文献借阅、咨询服务、科技查新：66554700 |