晋蒙地区西施沟复式岩体锆石U-Pb年龄、地球化学特征及岩石成因
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摘要
本文对晋蒙地区的西施沟复式岩体进行了LA-ICP-MS锆石U-Pb定年、岩石地球化学特征研究,探讨了其岩石成因及其对华北克拉通北缘中生代构造岩浆演化的启示。该岩体的岩石类型从中性岩至酸性岩连续变化且以中性岩为主,内部广泛发育微粒闪长质包体,具明显的岩浆混合成因;锆石U-Pb定年结果显示其形成年龄为160. 19±0. 50Ma,为中晚侏罗世岩浆活动的产物;岩石地球化学数据表明,属于准铝(弱过铝)质的高钾钙碱性系列I型花岗岩;稀土总量(ΣREE)中等,轻重稀土分馏明显,无明显负铕异常;均富集轻稀土及大离子亲石元素(Ba、Rb、K),亏损高场强元素(Nb、Ta、P),具明显的陆壳成分特征;其形成可能与中晚侏罗世古太平洋板块的俯冲有关,为华北板块陆内造山作用的产物。
In this work,LA-ICP-MS zircon U-Pb dating and geochemical characteristics of the Xishigou complex pluton across the border between Shanxi and Inner Mongolia were studied. Its petrogenesis and implications for Mesozoic tectonomagmatic evolution in the northern margin of North China Craton were discussed. The rock types vary from intermediate to acidic rocks,dominated by intermediate rocks. Microgranular mafic enclaves are widely developed in the pluton,indicative of an obvious magmatic mixing origin. Zircon U-Pb dating shows their formation ages at( 160. 19 ± 0. 50) Ma,indicating that they are the product of magmatic activity in the middle Late Jurassic. Geochemical data suggest that the pluton is a metaluminous to peraluminous I-type granite and belongs to the high-K calc-alkaline series. The rock has medium ΣREE and high fractionation degree of LREE and HREE,without pronounced negative Eu anomalies. It also exhibits LREE and LILE( Ba,Rb,K) enrichment,and HFSE( Nb,Ta,P) depletion. These features are similar to geochemical characteristics of continental crust composition. The formation of the pluton may be related to the subduction of the Pacific Plate in the middle Late Jurassic,a product of intracontinental orogeny in the North China plate.
In this work,LA-ICP-MS zircon U-Pb dating and geochemical characteristics of the Xishigou complex pluton across the border between Shanxi and Inner Mongolia were studied. Its petrogenesis and implications for Mesozoic tectonomagmatic evolution in the northern margin of North China Craton were discussed. The rock types vary from intermediate to acidic rocks,dominated by intermediate rocks. Microgranular mafic enclaves are widely developed in the pluton,indicative of an obvious magmatic mixing origin. Zircon U-Pb dating shows their formation ages at( 160. 19 ± 0. 50) Ma,indicating that they are the product of magmatic activity in the middle Late Jurassic. Geochemical data suggest that the pluton is a metaluminous to peraluminous I-type granite and belongs to the high-K calc-alkaline series. The rock has medium ΣREE and high fractionation degree of LREE and HREE,without pronounced negative Eu anomalies. It also exhibits LREE and LILE( Ba,Rb,K) enrichment,and HFSE( Nb,Ta,P) depletion. These features are similar to geochemical characteristics of continental crust composition. The formation of the pluton may be related to the subduction of the Pacific Plate in the middle Late Jurassic,a product of intracontinental orogeny in the North China plate.
引文
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Chen Bin,Liu Chaoqun,Tian Wei.2006.Magma mixing between mantle and crustal derived melts in process of Mesozoic magmatism,Taihangshan:Constrains from petrology and geochemistry[J].Earth Science Frontiers,13(2):140-147(in Chinese with English abstract).
Chen Bin,He Jingbo,Ma Xinghua.2009.Petrogenesis of mafic enclaves from the north Taihang Yanshanqi intermediate to felsic plutons:Evidence from petrological,geochemical and zircon Hf-O isotopic data[J].Science China,Series D-Earth Science,39(7):922-934(in Chinese with English abstract).
Chappell B W.1999.Aluminium saturation in I-and S-type granites and the characterization of fractionated haplogranites[J].Lithos,46(3):535-551.
Collins W J,Beams S D,White A J R,Chappel B W.1982.Nature and origin of A-type granites with particular reference to southeastern Australia[J].Contributions to Mineralogy and Petrology,80(2):189-200.
Deng Jinfu,Liu Cui,Feng Yanfang,Xiao Qinghui,You Yongjun,Su Shangguo,Zhao Guochun,Duan Peixin,Dai Meng.2015.On the correct application in the common igneous petrological diagrams:Discussion and suggestion[J].Geological Review,61(4):717-734(in Chinese with English abstract).
Ge Liangsheng,Wang Zhihua,Yang Guicai,Lu Yingchuan.2012.Yanshanian magmatism and gold-polymetallic mineralization dynamics in northeastern Shanxi Province,China[J].Acta Petrologica Sinica,28(2):619-636(in Chinese with English abstract).
He Zhenyu,Xu Xisheng,Niu Yaoling.2010.Petrogenesis and tectonic significance of a Mesozoic granite-syenite-gabbro association from inland South China[J].Lithos,119(3-4):621-641.
Kemp A I S,Hawkesworth C J,Foster G L,Paterson B A,Woodhead J D,Hergt J M,Gray C M,Whitehouse M J.2007.Magmatic and crustal differentiation history of granitic rocks from Hf-O isotopes in zircon[J].Science,315(5814):980-983.
King P L,White A J R,Chappell B W,Allen C M.1997.Characterization and origin of aluminous A-type granites from the Lachlan fold belt,southeastern Australia[J].Journal of Petrology,38(3):371-391.
Liu Hongtao,Sun Shihua,Liu Jianming,Zhai Mingguo.2002.The Mesozoic high-strontium granites in the northern margin of the North China Craton:Geochenistty and source-zone properties[J].Acta Petrologica Sinica,18(3):257-274(in Chinese with English abstract).
Le Maitre R W.2002.Igneous rocks:A classification and glossary of terms[J].2ndEdition.Cambridge:Cambridge University Press:33-39.
Li Shengyuan,Ma Xiaobing.1999.Crypto explosive rock and its oreforming sense to gold-silver deposit in the northeastern Shanxi Province,China[J].Contributions to Geology and Mineral Resources Research,14(4):8-14(in Chinese with English abstract).
Maniar P D,Piccoli P M.1989.Tectonic discrimination of granitoids[J].Geological Society of America Bulletin,101(5):635-643.
Morrison W G.1980.Characteristics and tectonic setting of the shoshonite rock association[J].Lithos,13(1):97-108.
Pearce,Harris,Tindle.1984.Trace element discrimination diagrams for the tectonic interpretation of granitic rocks[J].Journal of Petrology,25(4):956-983.
Pichavant M,Montel J M,Richard L R.1992.Apatite solubility in peraluminous liquiqs:Experimental data and an extension of the HarrisonWaston model[J].Geochimica et Cosmochimica Acta,56(10):3855-3861.
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Sun S S,Mc Donough W F.1989.Chemical and isotopic systematics of oceanic basalts:Implications for mantle composition and processes[J].Geological Society of London,Specical Publications,42(1):313-345.
Watson E B,Harrison T M.1983.Zircon saturation revisited:Temperature and composition effects in a variety of crustal magma types[J].Earth Planetary Science Letters,64(2):295-304.
Whalen J B,Currie K L,Chappell B W.1987.A-type granites:Geochemical characteristics discrimination and petrogenesis[J].Contributions to Mineralogy and Petrology,95(4):407-409.
Wu Fuyuan,Sun Deyou,Li Huimin,Jahn Borming,Wilde Simon.2002.A-type granites in northeastern China:Age and geochemical constraints on their petrogenesis[J].Chemical Geology,187(1-2):143-173.
Wu Fuyuan,Jahn B M,Wilder S A,Lo C H,Yui T F,Lin Qiang,Ge Wenchun,Sun Deyou.2003.Highly fractionated I-type granites in NEChina(I):Geochronology and petrogenesis[J].Lithos,66(3-4):241-273.
Wu Fuyuan,Li Xianhua,Yang Jinhui,Zheng Yongfei.2007.Discussions on the petrogenesis of granites[J].Acta Petrologica Sinica,23(6):1217-1238(in Chinese with English abstract).
Xu Bei,Chen Bin.1997.Frame work and evolution of the Middle Paleozoic orogenic belt between Siberian and North China Plate in northern Inner Mongolia[J].Science in China(Series D),40:463-469(in Chinese with English abstract)
Xiao W,Windley B F,Hao J.2003.Accretion leading to collision and the Permian Solonker suture,Inner Mongolia,China:Termination of the central Asian orogenic belt[J].Tectonics,22(6):1-20.
Xiao Qinghui.2002.The ways of investigation on granitoids[M].Beijing:Geological Publishing House:156-172(in Chinese).
Zhang Guangning,Deng Jun,Ye Jinhua,Sun Nuo,He Wenyan,Liu Jiangtao,Gao Xue.2015.Magma mixing in the Machangjing copperbearing alkali-rich porphyry of western Yunnan:Evidence of petrology and geochemistry[J].Geological and Exploration,51(4):599-609(in Chinese with English abstract).
Zhang Jianjun,Wang Tao,Zhang Zhaochong,Tong Ying,Zhang Lei,Shi Xingjun,Guo Lei,Li Shan,Zeng Tao.2012.Magma mixing origin of Yamatu granite in Nuoergong-Langshan area,western part of the northern margin of North China Craton:Petrological and geochemical evidences[J].Geological Review,58(1):53-66(in Chinese with English abstract).
Zhang Shuanhong,Zhao Yue,Hu Jianmin,Song Biao,Liu Jian,Wu Hai.2010.Geochronology,geochemistry and tectonic setting of the Late Paleozoic-Early Mesozoic magmatism in the northern margin of the North China Block:A preliminary review[J].Acta Petrologica et Mineralogica,29(6):824-842(in Chinese with English abstract).
Zhang Xuebin,Zhou Changhong,Lai Lin,Xu Cui,Tian Ying,Chen Lizhen,Wei Min.2015.Geochemistry and zircon U-Pb dating of volcanic rocks in eastern Xilin Hot,Inner Monglia and their geological implications[J].Geological and Exploration,51(2):290-302(in Chinese with English abstract).
Zhang Yusheng.1995.Geological characteristics of superunits in Zhuyangou,Inner Mongolia[J].Regional Geology of China,(4):304-308(in Chinese with English abstract).
Zhao Yumei,Peng Ge,Zhao Delong,You Yuecheng.2016.LA-ICP-MSzircon U-Pb age and geochemistry of the Kezile granitic pluton in Altay of China and their geological implications[J].Geological and Exploration,52(2):271-282(in Chinese with English abstract).
陈斌,田伟,翟明国,荒川洋二.2005.太行山和华北其他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[J].岩石学报,21(1):13-24.
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邓晋福,刘翠,冯艳芳,肖庆辉,狄永军,苏尚国,赵国春,段培新,戴蒙.2015.关于火成岩常用图解的正确使用:讨论与建议[J].地质与论评,61(4):717-734.
葛良胜,王治华,杨贵才,路英川.2012.晋东北燕山期岩浆活动与金多金属成矿作用动力学[J].岩石学报,28(2):619-636.
刘红涛,孙世华,刘建明,翟明国.2002.华北克拉通北缘中生代高锶花岗岩类:地球化学性质与源区性质[J].岩石学报,18(3):257-274.
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Chen Bin,Liu Chaoqun,Tian Wei.2006.Magma mixing between mantle and crustal derived melts in process of Mesozoic magmatism,Taihangshan:Constrains from petrology and geochemistry[J].Earth Science Frontiers,13(2):140-147(in Chinese with English abstract).
Chen Bin,He Jingbo,Ma Xinghua.2009.Petrogenesis of mafic enclaves from the north Taihang Yanshanqi intermediate to felsic plutons:Evidence from petrological,geochemical and zircon Hf-O isotopic data[J].Science China,Series D-Earth Science,39(7):922-934(in Chinese with English abstract).
Chappell B W.1999.Aluminium saturation in I-and S-type granites and the characterization of fractionated haplogranites[J].Lithos,46(3):535-551.
Collins W J,Beams S D,White A J R,Chappel B W.1982.Nature and origin of A-type granites with particular reference to southeastern Australia[J].Contributions to Mineralogy and Petrology,80(2):189-200.
Deng Jinfu,Liu Cui,Feng Yanfang,Xiao Qinghui,You Yongjun,Su Shangguo,Zhao Guochun,Duan Peixin,Dai Meng.2015.On the correct application in the common igneous petrological diagrams:Discussion and suggestion[J].Geological Review,61(4):717-734(in Chinese with English abstract).
Ge Liangsheng,Wang Zhihua,Yang Guicai,Lu Yingchuan.2012.Yanshanian magmatism and gold-polymetallic mineralization dynamics in northeastern Shanxi Province,China[J].Acta Petrologica Sinica,28(2):619-636(in Chinese with English abstract).
He Zhenyu,Xu Xisheng,Niu Yaoling.2010.Petrogenesis and tectonic significance of a Mesozoic granite-syenite-gabbro association from inland South China[J].Lithos,119(3-4):621-641.
Kemp A I S,Hawkesworth C J,Foster G L,Paterson B A,Woodhead J D,Hergt J M,Gray C M,Whitehouse M J.2007.Magmatic and crustal differentiation history of granitic rocks from Hf-O isotopes in zircon[J].Science,315(5814):980-983.
King P L,White A J R,Chappell B W,Allen C M.1997.Characterization and origin of aluminous A-type granites from the Lachlan fold belt,southeastern Australia[J].Journal of Petrology,38(3):371-391.
Liu Hongtao,Sun Shihua,Liu Jianming,Zhai Mingguo.2002.The Mesozoic high-strontium granites in the northern margin of the North China Craton:Geochenistty and source-zone properties[J].Acta Petrologica Sinica,18(3):257-274(in Chinese with English abstract).
Le Maitre R W.2002.Igneous rocks:A classification and glossary of terms[J].2ndEdition.Cambridge:Cambridge University Press:33-39.
Li Shengyuan,Ma Xiaobing.1999.Crypto explosive rock and its oreforming sense to gold-silver deposit in the northeastern Shanxi Province,China[J].Contributions to Geology and Mineral Resources Research,14(4):8-14(in Chinese with English abstract).
Maniar P D,Piccoli P M.1989.Tectonic discrimination of granitoids[J].Geological Society of America Bulletin,101(5):635-643.
Morrison W G.1980.Characteristics and tectonic setting of the shoshonite rock association[J].Lithos,13(1):97-108.
Pearce,Harris,Tindle.1984.Trace element discrimination diagrams for the tectonic interpretation of granitic rocks[J].Journal of Petrology,25(4):956-983.
Pichavant M,Montel J M,Richard L R.1992.Apatite solubility in peraluminous liquiqs:Experimental data and an extension of the HarrisonWaston model[J].Geochimica et Cosmochimica Acta,56(10):3855-3861.
Rudnick R L,Gao Shan.2003.Composition of the continental crust.In:Rudnick RL.(ed.)[J].Treatise on Geochemistry,Volume 3.Oxford:Elsevier:1-64.
Sun S S,Mc Donough W F.1989.Chemical and isotopic systematics of oceanic basalts:Implications for mantle composition and processes[J].Geological Society of London,Specical Publications,42(1):313-345.
Watson E B,Harrison T M.1983.Zircon saturation revisited:Temperature and composition effects in a variety of crustal magma types[J].Earth Planetary Science Letters,64(2):295-304.
Whalen J B,Currie K L,Chappell B W.1987.A-type granites:Geochemical characteristics discrimination and petrogenesis[J].Contributions to Mineralogy and Petrology,95(4):407-409.
Wu Fuyuan,Sun Deyou,Li Huimin,Jahn Borming,Wilde Simon.2002.A-type granites in northeastern China:Age and geochemical constraints on their petrogenesis[J].Chemical Geology,187(1-2):143-173.
Wu Fuyuan,Jahn B M,Wilder S A,Lo C H,Yui T F,Lin Qiang,Ge Wenchun,Sun Deyou.2003.Highly fractionated I-type granites in NEChina(I):Geochronology and petrogenesis[J].Lithos,66(3-4):241-273.
Wu Fuyuan,Li Xianhua,Yang Jinhui,Zheng Yongfei.2007.Discussions on the petrogenesis of granites[J].Acta Petrologica Sinica,23(6):1217-1238(in Chinese with English abstract).
Xu Bei,Chen Bin.1997.Frame work and evolution of the Middle Paleozoic orogenic belt between Siberian and North China Plate in northern Inner Mongolia[J].Science in China(Series D),40:463-469(in Chinese with English abstract)
Xiao W,Windley B F,Hao J.2003.Accretion leading to collision and the Permian Solonker suture,Inner Mongolia,China:Termination of the central Asian orogenic belt[J].Tectonics,22(6):1-20.
Xiao Qinghui.2002.The ways of investigation on granitoids[M].Beijing:Geological Publishing House:156-172(in Chinese).
Zhang Guangning,Deng Jun,Ye Jinhua,Sun Nuo,He Wenyan,Liu Jiangtao,Gao Xue.2015.Magma mixing in the Machangjing copperbearing alkali-rich porphyry of western Yunnan:Evidence of petrology and geochemistry[J].Geological and Exploration,51(4):599-609(in Chinese with English abstract).
Zhang Jianjun,Wang Tao,Zhang Zhaochong,Tong Ying,Zhang Lei,Shi Xingjun,Guo Lei,Li Shan,Zeng Tao.2012.Magma mixing origin of Yamatu granite in Nuoergong-Langshan area,western part of the northern margin of North China Craton:Petrological and geochemical evidences[J].Geological Review,58(1):53-66(in Chinese with English abstract).
Zhang Shuanhong,Zhao Yue,Hu Jianmin,Song Biao,Liu Jian,Wu Hai.2010.Geochronology,geochemistry and tectonic setting of the Late Paleozoic-Early Mesozoic magmatism in the northern margin of the North China Block:A preliminary review[J].Acta Petrologica et Mineralogica,29(6):824-842(in Chinese with English abstract).
Zhang Xuebin,Zhou Changhong,Lai Lin,Xu Cui,Tian Ying,Chen Lizhen,Wei Min.2015.Geochemistry and zircon U-Pb dating of volcanic rocks in eastern Xilin Hot,Inner Monglia and their geological implications[J].Geological and Exploration,51(2):290-302(in Chinese with English abstract).
Zhang Yusheng.1995.Geological characteristics of superunits in Zhuyangou,Inner Mongolia[J].Regional Geology of China,(4):304-308(in Chinese with English abstract).
Zhao Yumei,Peng Ge,Zhao Delong,You Yuecheng.2016.LA-ICP-MSzircon U-Pb age and geochemistry of the Kezile granitic pluton in Altay of China and their geological implications[J].Geological and Exploration,52(2):271-282(in Chinese with English abstract).
陈斌,田伟,翟明国,荒川洋二.2005.太行山和华北其他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[J].岩石学报,21(1):13-24.
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[J].地学前缘,13(2):140-147.
陈斌,贺敬博,马星华.2009.北太行山燕山期中酸性岩体中暗色包体的成因:岩石学、地球化学和锆石Hf-O同位素证据[J].中国科学D辑:地球科学,39(7):922-934.
邓晋福,刘翠,冯艳芳,肖庆辉,狄永军,苏尚国,赵国春,段培新,戴蒙.2015.关于火成岩常用图解的正确使用:讨论与建议[J].地质与论评,61(4):717-734.
葛良胜,王治华,杨贵才,路英川.2012.晋东北燕山期岩浆活动与金多金属成矿作用动力学[J].岩石学报,28(2):619-636.
刘红涛,孙世华,刘建明,翟明国.2002.华北克拉通北缘中生代高锶花岗岩类:地球化学性质与源区性质[J].岩石学报,18(3):257-274.
李生元,马小兵.1999.晋东北引爆岩及其对金银的控矿意义[J].地质找矿论丛,14(4):8-14.
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