辽东黄泥岭石英二长岩锆石U--Pb年代学、岩石地球化学及其成因
|
摘要
对华北克拉通东北缘、辽东黄泥岭岩体锆石U--Pb年代学和岩石地球化学的测试研究表明,黄泥岭岩体岩性为似斑状含辉石石英二长岩,锆石U--Pb加权平均年龄为174±0. 4 Ma,成岩时代为中侏罗世早期;岩石主量元素具有高Al、Ca、Na、Fe,低Mg特征;δEu弱-无负异常;富集Rb、Sr、Ba、Th、U等大离子亲石元素和LREE,亏损高场强元素Nb、Ta、Zr、Hf、Ti、HREE和相容元素V、Cr、Co、Ni,为"高Sr低Yb型"花岗岩。黄泥岭岩体为C型埃达克质岩,其岩浆来自于加厚基性下地壳的部分熔融。黄泥岭石英二长岩等中侏罗世早期C型埃达克质岩在华北克拉通东缘的大量分布表明,至少从中侏罗世初开始,古亚洲洋构造体系对本区的控制已经结束,环太平洋构造体系主导了本区的构造岩浆活动。
Through petrogeochemistry,zircon U--Pb geochronology in Huangniling pluton from the northeastern margin of North China craton,it is indicated that the Huangniling pluton is composed of pyroxene adamellite. It formed during the Early Middle Jurassic with a weighted mean age of 174 ± 0. 4 Ma. The major elements of the adamellite are characterized by high Al,Ca,Na,Fe and low Mg,with negligible Eu anomalies. Huangniling pluton is enriched in large ion lithophile elements( LILE)( e. g.,Rb,Sr,Ba,Th,U and LREE),and depleted in high field strength elements( HFSE)( e. g.,Nb,Ta,Zr,Hf,Ti and HREE) and compatible element V,Cr,Co and Ni. The adamellite in Huangniling belongs to C-type adakite with high Sr and low Yb. The Huangniling pluton magma was derived mainly from partial melting of mafic rocks in thickened lower crust. The wide distribution of the Middle Jurassic C-type Adakite in the eastern margin of the North China craton,such as the Huanglinlingadamellite,indicates that at least since Middle Jurassic,the control of the Paleo--Asian ocean tectonic system on the study area has ended. The circum-Pacific tectonic system dominates the structural magmatism in this area.
Through petrogeochemistry,zircon U--Pb geochronology in Huangniling pluton from the northeastern margin of North China craton,it is indicated that the Huangniling pluton is composed of pyroxene adamellite. It formed during the Early Middle Jurassic with a weighted mean age of 174 ± 0. 4 Ma. The major elements of the adamellite are characterized by high Al,Ca,Na,Fe and low Mg,with negligible Eu anomalies. Huangniling pluton is enriched in large ion lithophile elements( LILE)( e. g.,Rb,Sr,Ba,Th,U and LREE),and depleted in high field strength elements( HFSE)( e. g.,Nb,Ta,Zr,Hf,Ti and HREE) and compatible element V,Cr,Co and Ni. The adamellite in Huangniling belongs to C-type adakite with high Sr and low Yb. The Huangniling pluton magma was derived mainly from partial melting of mafic rocks in thickened lower crust. The wide distribution of the Middle Jurassic C-type Adakite in the eastern margin of the North China craton,such as the Huanglinlingadamellite,indicates that at least since Middle Jurassic,the control of the Paleo--Asian ocean tectonic system on the study area has ended. The circum-Pacific tectonic system dominates the structural magmatism in this area.
引文
[1]李锦轶,高立明,孙桂华,等.内蒙古东部双井子中三叠世同碰撞壳源花岗岩的确定及其对西伯利亚与中朝古板块碰撞时限的约束[J].岩石学报,2007,23(3):565-582.LI Jin-yi, GAO Li-ming, SUN Gui-hua, et al.Shuangjingzi Middle Triassic syn-collisional crust-derived granite in the east Inner Mongolia and its constraint on the timing of collision between Siberian and Sino-Korean paleo-plates[J]. Acta Petrologica Sinica, 2007, 23(3):565-582.
[2]刘建峰,李锦轶,孙立新,等.内蒙古巴林左旗九井子蛇绿岩锆石U--Pb定年:对西拉木伦河缝合带形成演化的约束[J].中国地质,2016,43(6):1947-1962.LIU Jian-feng,LI Jin-yi,SUN Li-xin,et al. Zircon U--Pb dating of the Jiujingzi ophiolite in Bairin Left Banner,Inner Mongolia:constraints on the formation and evolution of the Xar Moron River suture zone[J]. Geology in China,2016,43(6):1947-1962.
[3]王成文,金巍,张兴洲,等.东北及邻区晚古生代大地构造属性新认识[J].地层学杂志,2008,32(2):119-136.WANG Cheng-wen, JIN Wei, ZHANG Xing-zhou, et al. New understanding of the Late Paleozoic tectonics in northeastern China and adjacent areas[J]. Journal of Stratigraphy,2008,32(2):119-136.
[4] Wu F Y,Zhao G C,Sun D Y,et al. The Hulan Group:its role in the evolution of the central Asian Orogenic Belt of NE China[J]. Journal of Asian Earth Sciences,2007,30(3):542-556.
[5] Yang J H,Wu F Y. Triassic magmatism and its relation to decratonization in the eastern North China Craton[J].Science in China,2009,52(9):1319-1330.
[6]邵济安,刘福田,陈辉,等.大兴安岭-燕山晚中生代岩浆活动与俯冲作用关系[J].地质学报,2001,75(1):56-63.SHAO Ji-an,LIU Fu-tian,CHEN Hui,et al. Relationship between Late Mesozoic magmatism and subduction in the Daxingan Mountains-Yanshan Mountains[J]. Acta Geologica Sinica,2001,75(1):56-63.
[7] Maruyama S,Send T. Orogeny and relative plate motions:example of the Japanese Islands[J]. Tectonophysics,1986,127(3):305-329.
[8] Maruyama S,Isozaki Y,Kimura G,et al. Paleogeographic maps of the Japanese Islands:plate tectonic synthesis from 750 Ma to the present[J]. Island Arc,2010,6(1):121-142.
[9]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[J].现代地质,1994,8(3):349-356.DENG Jin-fu,MO Xuan-xue, ZHAO Hai-ling, et al.Lithosphere root/de-rooting and activation of the East China continent[J]. Geoscience,1994,8(3):349-356.
[10]邓晋福,刘厚祥.燕辽地区燕山期火成岩与造山模型[J].现代地质,1996,10(2):137-148.DENG Jin-fu,LIU Hou-xiang. The Yanshan stage igneous rock and orogenic model in Yanliao area[J]. Modern Geology,1996,10(2):137-148.
[11]吴福元,曹林.东北亚地区的若干重要基础地质问题[J].世界地质,1999,18(2):1-13.WU Fu-yuan,CAO Lin. Some important basic geological problems in Northeast Asia[J]. Global Geology,1999,18(2):1-13.
[12]吴福元,孙德有.东北地区显生宙花岗岩的成因与地壳增生[J].岩石学报,1999,15(2):181-189.WU Fu-yuan,SUN De-you. Petrogenesis of the Phanerozoic granites and crustal growth in Northeast China[J]. Acta Petrologica Sinica,1999,15(2):181-189.
[13]张旗,王焰,钱青,等.中国东部燕山期埃达克岩的特征及其构造—成矿意义[J].岩石学报,2001,17(2):236-244.ZHANG Qi, WANG Yan, QIAN Qing, et al. The characteristics and tectonic-metallogenic significances of the adakites in Yanshan period from eastern China[J].Acta Petrologica Sinica,2001,17(2):236-244.
[14]张旗,王焰,王元龙.燕山期中国东部高原下地壳组成初探:埃达克质岩Sr、Nd同位素制约[J].岩石学报,2001,17(4):505-513.ZHANG Qi,WANG Yan,WANG Yuan-long. Preliminary study of lower crust composition in eastern Yanshan Plateau:Sr and Nd isotopic constraints of the adakite rocks[J]. Acta Petrologica Sinica,2001,17(4):505-513.
[15]翟明国,樊祺诚.华北克拉通中生代下地壳置换:非造山过程的壳幔交换[J].岩石学报,2002,18(1):1-8.ZHAI Ming-guo,FAN Qi-cheng. Mesozoic replacement of bottom crust in North China Craton:anorogenic mantle-crust interaction[J]. Acta Petrologica Sinica,2002,18(1):1-8.
[16]邵济安,韩庆军,张履桥,等.陆壳垂向增生的两种方式:以大兴安岭为例[J].岩石学报,1999,15(4):600-606.SHAO Ji-an,HAN Qing-jun,ZHANG Lu-qiao,et al.Two ways of vertical accretion of continental crust:take Greater Khingan Range as an example[J]. Acta Petrologica Sinica,1999,15(4):600-606.
[17]吴福元,杨进辉,柳小明.辽东半岛中生代花岗质岩浆作用的年代学格架[J].高校地质学报,2005,11(3):305-317.WU Fu-yuan, YANG Jin-hui, LIU Xiao-ming. Geochronological framework of the Mesozoic granite mag-matism in the Liaodong Peninsula,Northeast China[J].Geological Journal of China Universities, 2005, 11(3):305-317.
[18]孙德有,吴福元,张艳斌,等.西拉木伦河—长春—延吉板块缝合带的最后闭合时间:来自吉林大玉山花岗岩体的证据[J].吉林大学学报(地球科学版),2004,34(2):174-181.SUN De-you,WU Fu-yuan,ZHANG Yan-bin,et al.The final closing time of the west Lamulun River--Changchun--Yanji plate suture zone-evidence from the Dayushan granitic pluton,Jilin Province[J]. Journal of Jilin University(Earth Science Edition),2004,34(2):174-181.
[19]孙德有,吴福元,高山,等.吉林中部晚三叠世和早侏罗世两期铝质A型花岗岩的厘定及对吉黑东部构造格局的制约[J].地学前缘,2005,12(2):265-277.SUN De-you,WU Fu-yuan,GAO Shan,et al. Confirmation of two episodes of A-type granite emplacement during Late Triassic and Early Jurassic in the central Jilin Province,and their constraints on the structural pattern of eastern Jilin-Heilongjiang area, China[J].Earth Science Frontiers,2005,12(2):265-277.
[20]裴福萍,许文良,于洋,等.吉林南部晚三叠世蚂蚁河岩体的成因:锆石U--Pb年代学和地球化学证据[J].吉林大学学报(地球科学版),2008,38(3):351-362.PEI Fu-ping,XU Wen-liang,YU Yang,et al. Petrogenesis of the Late Triassic Mayihe Pluton in southern Jilin Province:evidence from zircon U--Pb geochronology and geochemistry[J]. Journal of Jilin University(Earth Science Edition),2008,38(3):351-362.
[21]杨进辉,吴福元,罗清华,等.辽宁丹东地区侏罗纪花岗岩的变形时代:40Ar/39Ar年代学制约[J].岩石学报,2004,20(5):1205-1214.YANG Jin-hui,WU Fu-yuan,LUO Qing-hua,et al.Deformation age of Jurassic granites in the Dandong area,eastern China:40Ar/39Ar geochronological constraints[J]. Actor Petrologica Sinica,2004,20(5):1205-1214.
[22]郭春丽,吴福元,杨进辉,等.中国东部早白垩世岩浆作用的伸展构造性质:以辽东半岛南部饮马湾山岩体为例[J].岩石学报,2004,20(5):1193-1204.GUO Chun-li, WU Fu-yuan, YANG Jin-hui, et al.The extensional setting of the Early Cretaceous magmatism in eastern China:example from the Yinmawanshan pluton in southern Liaodong Peninsula[J]. Acta Petrologica Sinica,2004,20(5):1193-1204.
[23]李三忠,刘建忠,赵国春,等.华北克拉通东部地块中生代变形的关键时限及其对构造的制约:以胶辽地区为例[J].岩石学报,2004,20(3):633-646.LI San-zhong, LIU Jian-zhong, ZHAO Guo-chun, et al. Key geochronology of Mesozoic deformation in the eastern block of the North China Craton and its constraints on regional tectonics:a case of Jiaodong and Liaodong Peninsula[J]. Acta Petrologica Sinica,2004,20(3):633-646.
[24]杨进辉,吴福元,邵济安,等.冀北张—宣地区后城组、张家口组火山岩锆石U--Pb年龄和Hf同位素[J].地球科学,2006,31(1):75-84.YANG Jin-hui,WU Fu-yuan,SHAO Ji-an,et al. Insitu U--Pb dating and Hf isotopic analyses of zircons from volcanic rocks of the Houcheng and Zhangjiakou formations in the Zhang-Xuan area,Northeast China[J].Earth Science,2006,31(1):75-84.
[25]秦亚,梁一鸿,邢济麟,等.内蒙古正镶白旗地区早古生代O型埃达克岩的厘定及其意义[J].地学前缘,2013,20(5):106-114.QIN Ya,LIANG Yi-hong,XING Ji-lin,et al. The identification of Early Paleozoic O-type adakitic rocks in Zhengxiangbaiqi area, Inner Mongolia and its significance[J]. Earth Science Frontiers,2013,20(5):106-114.
[26] Taylor S R,McLennan S M. The continental crust:its composition and evolution[M]. Oxford:Blackwell Scientific Publications,1985:54-372.
[27]杨进辉,吴福元,柳小明,等.辽东半岛小黑山岩体成因及其地质意义:锆石U--Pb年龄和铪同位素证据[J].矿物岩石地球化学通报,2007,26(1):29-43.YANG Jin-hui,WU Fu-yuan,LIU Xiao-ming,et al.Petrogenesis and geological significance of the Jurassic Xiaoheishan Pluton in the Liaodong Peninsula, East China:In-situ zircon U--Pb dating and Hf isotopic analysis[J]. Bulletin of Mineralogy,Petrology and Geochemistry,2007,26(1):29-43.
[28]孙德有,铃木和博,吴福元,等.吉林省南部荒沟山地区中生代花岗岩CHIME定年[J].地球化学,2005,34(4):305-310.SUN De-you,Suzuki K,WU Fu-yuan,et al. CHIME dating and its application for Mesozoic granites of Huanggoushan, Jilin Province[J]. Geochimica,2005,34(4):305-310.
[29]张超,郭巍,徐仲元,等.吉林东部延边地区二长花岗岩年代学、岩石成因学及其构造意义研究[J].岩石学报,2014,30(2):512-526.ZHANG Chao, GUO Wei, XU Zhong-yuan, et al.Study on geochronology,petrogenesis and tectonic implications of monzogranite from the Yanbian area,eastern Jilin Province[J]. Acta Petrologica Sinica,2014,30(2):512-526.
[30] Defant M J,Drummond M S. Derivation of some modern arc magmas by melting of young subducted lithosphere[J]. Nature,1990,347(6294):662-665.
[31] Castillo P R. An overview of adakite petrogenesis[J].Chinese Science Bulletin,2006,51(3):4-14.
[32]张旗,许继峰,王焰,等.埃达克岩的多样性[J].地质通报,2004,23(9):959-965.ZHANG Qi,XU Ji-feng,WANG Yan,et al. Diversity of adakite[J]. Geological Bulletin of China,2004,23(9):959-965.
[33] Condie K C. Earth systems-earth as an evolving planetary system[J]. Earth as an Evolving Planetary System,2005,15(4):1-11.
[34] Xu J F,Shinjo R,Defant M J,et al. Origin of Mesozoic adakitic intrusive rock in the Ningzhen area of east China:partial melting of delaminated lower continental crust?[J]. Geology,2002,30(12):1111-1114.
[35] Sheppard S,Griffin T J,Tyler I M,et al. High-and low-K granites and adakites at a Palaeoproterozoic plate boundary in northwestern Australia[J]. Journal of the Geological Society,2001,158(3):547-560.
[36] Altherr R,Holl A,Hegner E,et al. High-potassium,calc-alkaline I-type plutonism in the European Variscides:northern Vosges(France)and northern Schwarzwald(Germany)[J]. Lithos,2000,50(1):51-73.
[37]孙如江,孙德有,苟军,等.大兴安岭北部新林石英二长岩-花岗岩的地球化学特征及其成因[J].世界地质,2016,35(2):309-323.SUN Ru-jiang,SUN De-you,GOU Jun,et al. Geochemical characteristics and petrogenesis of adamellitegranite[J]. Global Geology,2016,35(2):309-323.
[38]齐成栋,纪春华,韩江,等.吉林省敦化地区晚三叠世碱性-亚碱性侵入杂岩体的地质特征及构造背景分析[J].吉林地质,2003,22(3):13-19.QI Cheng-dong,JI Chun-hua,HAN Jiang,et al. The geologic features of the Late Triassic alkali-meta-alkaliintrusive complex body of the Dunhua area,Jilin Province and its structural setting[J]. Jilin Geology,2003,22(3):13-19.
[39]孙晓,郭支涛,窦鲁文,等.黑龙江尚志一面坡固安屯组火山碎屑岩LA--ICP--MS锆石U--Pb定年和岩石化学特征[J].世界地质,2016,35(1):28-39.SUN Xiao,GUO Zhi-tao,DOU Lu-wen,et al. LAICP--MS zircon U--Pb dating and geochemical characteristics of volcano clastic rocks in Gu'antun Formation of Yimianpo of Shangzhi, Heilongjiang Province[J].Global Geology,2016,35(1):28-39.
[2]刘建峰,李锦轶,孙立新,等.内蒙古巴林左旗九井子蛇绿岩锆石U--Pb定年:对西拉木伦河缝合带形成演化的约束[J].中国地质,2016,43(6):1947-1962.LIU Jian-feng,LI Jin-yi,SUN Li-xin,et al. Zircon U--Pb dating of the Jiujingzi ophiolite in Bairin Left Banner,Inner Mongolia:constraints on the formation and evolution of the Xar Moron River suture zone[J]. Geology in China,2016,43(6):1947-1962.
[3]王成文,金巍,张兴洲,等.东北及邻区晚古生代大地构造属性新认识[J].地层学杂志,2008,32(2):119-136.WANG Cheng-wen, JIN Wei, ZHANG Xing-zhou, et al. New understanding of the Late Paleozoic tectonics in northeastern China and adjacent areas[J]. Journal of Stratigraphy,2008,32(2):119-136.
[4] Wu F Y,Zhao G C,Sun D Y,et al. The Hulan Group:its role in the evolution of the central Asian Orogenic Belt of NE China[J]. Journal of Asian Earth Sciences,2007,30(3):542-556.
[5] Yang J H,Wu F Y. Triassic magmatism and its relation to decratonization in the eastern North China Craton[J].Science in China,2009,52(9):1319-1330.
[6]邵济安,刘福田,陈辉,等.大兴安岭-燕山晚中生代岩浆活动与俯冲作用关系[J].地质学报,2001,75(1):56-63.SHAO Ji-an,LIU Fu-tian,CHEN Hui,et al. Relationship between Late Mesozoic magmatism and subduction in the Daxingan Mountains-Yanshan Mountains[J]. Acta Geologica Sinica,2001,75(1):56-63.
[7] Maruyama S,Send T. Orogeny and relative plate motions:example of the Japanese Islands[J]. Tectonophysics,1986,127(3):305-329.
[8] Maruyama S,Isozaki Y,Kimura G,et al. Paleogeographic maps of the Japanese Islands:plate tectonic synthesis from 750 Ma to the present[J]. Island Arc,2010,6(1):121-142.
[9]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[J].现代地质,1994,8(3):349-356.DENG Jin-fu,MO Xuan-xue, ZHAO Hai-ling, et al.Lithosphere root/de-rooting and activation of the East China continent[J]. Geoscience,1994,8(3):349-356.
[10]邓晋福,刘厚祥.燕辽地区燕山期火成岩与造山模型[J].现代地质,1996,10(2):137-148.DENG Jin-fu,LIU Hou-xiang. The Yanshan stage igneous rock and orogenic model in Yanliao area[J]. Modern Geology,1996,10(2):137-148.
[11]吴福元,曹林.东北亚地区的若干重要基础地质问题[J].世界地质,1999,18(2):1-13.WU Fu-yuan,CAO Lin. Some important basic geological problems in Northeast Asia[J]. Global Geology,1999,18(2):1-13.
[12]吴福元,孙德有.东北地区显生宙花岗岩的成因与地壳增生[J].岩石学报,1999,15(2):181-189.WU Fu-yuan,SUN De-you. Petrogenesis of the Phanerozoic granites and crustal growth in Northeast China[J]. Acta Petrologica Sinica,1999,15(2):181-189.
[13]张旗,王焰,钱青,等.中国东部燕山期埃达克岩的特征及其构造—成矿意义[J].岩石学报,2001,17(2):236-244.ZHANG Qi, WANG Yan, QIAN Qing, et al. The characteristics and tectonic-metallogenic significances of the adakites in Yanshan period from eastern China[J].Acta Petrologica Sinica,2001,17(2):236-244.
[14]张旗,王焰,王元龙.燕山期中国东部高原下地壳组成初探:埃达克质岩Sr、Nd同位素制约[J].岩石学报,2001,17(4):505-513.ZHANG Qi,WANG Yan,WANG Yuan-long. Preliminary study of lower crust composition in eastern Yanshan Plateau:Sr and Nd isotopic constraints of the adakite rocks[J]. Acta Petrologica Sinica,2001,17(4):505-513.
[15]翟明国,樊祺诚.华北克拉通中生代下地壳置换:非造山过程的壳幔交换[J].岩石学报,2002,18(1):1-8.ZHAI Ming-guo,FAN Qi-cheng. Mesozoic replacement of bottom crust in North China Craton:anorogenic mantle-crust interaction[J]. Acta Petrologica Sinica,2002,18(1):1-8.
[16]邵济安,韩庆军,张履桥,等.陆壳垂向增生的两种方式:以大兴安岭为例[J].岩石学报,1999,15(4):600-606.SHAO Ji-an,HAN Qing-jun,ZHANG Lu-qiao,et al.Two ways of vertical accretion of continental crust:take Greater Khingan Range as an example[J]. Acta Petrologica Sinica,1999,15(4):600-606.
[17]吴福元,杨进辉,柳小明.辽东半岛中生代花岗质岩浆作用的年代学格架[J].高校地质学报,2005,11(3):305-317.WU Fu-yuan, YANG Jin-hui, LIU Xiao-ming. Geochronological framework of the Mesozoic granite mag-matism in the Liaodong Peninsula,Northeast China[J].Geological Journal of China Universities, 2005, 11(3):305-317.
[18]孙德有,吴福元,张艳斌,等.西拉木伦河—长春—延吉板块缝合带的最后闭合时间:来自吉林大玉山花岗岩体的证据[J].吉林大学学报(地球科学版),2004,34(2):174-181.SUN De-you,WU Fu-yuan,ZHANG Yan-bin,et al.The final closing time of the west Lamulun River--Changchun--Yanji plate suture zone-evidence from the Dayushan granitic pluton,Jilin Province[J]. Journal of Jilin University(Earth Science Edition),2004,34(2):174-181.
[19]孙德有,吴福元,高山,等.吉林中部晚三叠世和早侏罗世两期铝质A型花岗岩的厘定及对吉黑东部构造格局的制约[J].地学前缘,2005,12(2):265-277.SUN De-you,WU Fu-yuan,GAO Shan,et al. Confirmation of two episodes of A-type granite emplacement during Late Triassic and Early Jurassic in the central Jilin Province,and their constraints on the structural pattern of eastern Jilin-Heilongjiang area, China[J].Earth Science Frontiers,2005,12(2):265-277.
[20]裴福萍,许文良,于洋,等.吉林南部晚三叠世蚂蚁河岩体的成因:锆石U--Pb年代学和地球化学证据[J].吉林大学学报(地球科学版),2008,38(3):351-362.PEI Fu-ping,XU Wen-liang,YU Yang,et al. Petrogenesis of the Late Triassic Mayihe Pluton in southern Jilin Province:evidence from zircon U--Pb geochronology and geochemistry[J]. Journal of Jilin University(Earth Science Edition),2008,38(3):351-362.
[21]杨进辉,吴福元,罗清华,等.辽宁丹东地区侏罗纪花岗岩的变形时代:40Ar/39Ar年代学制约[J].岩石学报,2004,20(5):1205-1214.YANG Jin-hui,WU Fu-yuan,LUO Qing-hua,et al.Deformation age of Jurassic granites in the Dandong area,eastern China:40Ar/39Ar geochronological constraints[J]. Actor Petrologica Sinica,2004,20(5):1205-1214.
[22]郭春丽,吴福元,杨进辉,等.中国东部早白垩世岩浆作用的伸展构造性质:以辽东半岛南部饮马湾山岩体为例[J].岩石学报,2004,20(5):1193-1204.GUO Chun-li, WU Fu-yuan, YANG Jin-hui, et al.The extensional setting of the Early Cretaceous magmatism in eastern China:example from the Yinmawanshan pluton in southern Liaodong Peninsula[J]. Acta Petrologica Sinica,2004,20(5):1193-1204.
[23]李三忠,刘建忠,赵国春,等.华北克拉通东部地块中生代变形的关键时限及其对构造的制约:以胶辽地区为例[J].岩石学报,2004,20(3):633-646.LI San-zhong, LIU Jian-zhong, ZHAO Guo-chun, et al. Key geochronology of Mesozoic deformation in the eastern block of the North China Craton and its constraints on regional tectonics:a case of Jiaodong and Liaodong Peninsula[J]. Acta Petrologica Sinica,2004,20(3):633-646.
[24]杨进辉,吴福元,邵济安,等.冀北张—宣地区后城组、张家口组火山岩锆石U--Pb年龄和Hf同位素[J].地球科学,2006,31(1):75-84.YANG Jin-hui,WU Fu-yuan,SHAO Ji-an,et al. Insitu U--Pb dating and Hf isotopic analyses of zircons from volcanic rocks of the Houcheng and Zhangjiakou formations in the Zhang-Xuan area,Northeast China[J].Earth Science,2006,31(1):75-84.
[25]秦亚,梁一鸿,邢济麟,等.内蒙古正镶白旗地区早古生代O型埃达克岩的厘定及其意义[J].地学前缘,2013,20(5):106-114.QIN Ya,LIANG Yi-hong,XING Ji-lin,et al. The identification of Early Paleozoic O-type adakitic rocks in Zhengxiangbaiqi area, Inner Mongolia and its significance[J]. Earth Science Frontiers,2013,20(5):106-114.
[26] Taylor S R,McLennan S M. The continental crust:its composition and evolution[M]. Oxford:Blackwell Scientific Publications,1985:54-372.
[27]杨进辉,吴福元,柳小明,等.辽东半岛小黑山岩体成因及其地质意义:锆石U--Pb年龄和铪同位素证据[J].矿物岩石地球化学通报,2007,26(1):29-43.YANG Jin-hui,WU Fu-yuan,LIU Xiao-ming,et al.Petrogenesis and geological significance of the Jurassic Xiaoheishan Pluton in the Liaodong Peninsula, East China:In-situ zircon U--Pb dating and Hf isotopic analysis[J]. Bulletin of Mineralogy,Petrology and Geochemistry,2007,26(1):29-43.
[28]孙德有,铃木和博,吴福元,等.吉林省南部荒沟山地区中生代花岗岩CHIME定年[J].地球化学,2005,34(4):305-310.SUN De-you,Suzuki K,WU Fu-yuan,et al. CHIME dating and its application for Mesozoic granites of Huanggoushan, Jilin Province[J]. Geochimica,2005,34(4):305-310.
[29]张超,郭巍,徐仲元,等.吉林东部延边地区二长花岗岩年代学、岩石成因学及其构造意义研究[J].岩石学报,2014,30(2):512-526.ZHANG Chao, GUO Wei, XU Zhong-yuan, et al.Study on geochronology,petrogenesis and tectonic implications of monzogranite from the Yanbian area,eastern Jilin Province[J]. Acta Petrologica Sinica,2014,30(2):512-526.
[30] Defant M J,Drummond M S. Derivation of some modern arc magmas by melting of young subducted lithosphere[J]. Nature,1990,347(6294):662-665.
[31] Castillo P R. An overview of adakite petrogenesis[J].Chinese Science Bulletin,2006,51(3):4-14.
[32]张旗,许继峰,王焰,等.埃达克岩的多样性[J].地质通报,2004,23(9):959-965.ZHANG Qi,XU Ji-feng,WANG Yan,et al. Diversity of adakite[J]. Geological Bulletin of China,2004,23(9):959-965.
[33] Condie K C. Earth systems-earth as an evolving planetary system[J]. Earth as an Evolving Planetary System,2005,15(4):1-11.
[34] Xu J F,Shinjo R,Defant M J,et al. Origin of Mesozoic adakitic intrusive rock in the Ningzhen area of east China:partial melting of delaminated lower continental crust?[J]. Geology,2002,30(12):1111-1114.
[35] Sheppard S,Griffin T J,Tyler I M,et al. High-and low-K granites and adakites at a Palaeoproterozoic plate boundary in northwestern Australia[J]. Journal of the Geological Society,2001,158(3):547-560.
[36] Altherr R,Holl A,Hegner E,et al. High-potassium,calc-alkaline I-type plutonism in the European Variscides:northern Vosges(France)and northern Schwarzwald(Germany)[J]. Lithos,2000,50(1):51-73.
[37]孙如江,孙德有,苟军,等.大兴安岭北部新林石英二长岩-花岗岩的地球化学特征及其成因[J].世界地质,2016,35(2):309-323.SUN Ru-jiang,SUN De-you,GOU Jun,et al. Geochemical characteristics and petrogenesis of adamellitegranite[J]. Global Geology,2016,35(2):309-323.
[38]齐成栋,纪春华,韩江,等.吉林省敦化地区晚三叠世碱性-亚碱性侵入杂岩体的地质特征及构造背景分析[J].吉林地质,2003,22(3):13-19.QI Cheng-dong,JI Chun-hua,HAN Jiang,et al. The geologic features of the Late Triassic alkali-meta-alkaliintrusive complex body of the Dunhua area,Jilin Province and its structural setting[J]. Jilin Geology,2003,22(3):13-19.
[39]孙晓,郭支涛,窦鲁文,等.黑龙江尚志一面坡固安屯组火山碎屑岩LA--ICP--MS锆石U--Pb定年和岩石化学特征[J].世界地质,2016,35(1):28-39.SUN Xiao,GUO Zhi-tao,DOU Lu-wen,et al. LAICP--MS zircon U--Pb dating and geochemical characteristics of volcano clastic rocks in Gu'antun Formation of Yimianpo of Shangzhi, Heilongjiang Province[J].Global Geology,2016,35(1):28-39.