冀东青龙-双山子地区新太古代高镁安山岩-镁闪长岩锆石U-Pb年代学、地球化学及大地构造意义
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摘要
冀东地区位于华北克拉通北缘,学术界对该地区新太古代岩浆作用的成因模式及构造背景一直存在争议,因此对冀东青龙-双山子地区的新太古代变质表壳岩及侵入岩进行了系统的同位素年代学及岩石地球化学研究.锆石LA-MC-ICP-MS U-Pb年代学结果显示变安山岩的形成时代为2 576Ma,辉长闪长岩-英云闪长岩-石英闪长岩的侵入时代为2 484～2 535Ma.岩石地球化学特征显示,较早期的变安山岩部分属高镁安山岩类,源自俯冲板片脱水流体交代地幔楔的部分熔融;而稍晚的侵入岩类为具有埃达克质岩石特征的镁闪长岩类,源区具有熔体交代地幔楔部分熔融的特征;整体构成高镁安山岩-埃达克质镁闪长岩组合.结合区域上的同位素年代学及地球化学报道,冀东青龙-双山子地区新太古代应处于活动大陆边缘构造背景.
Eastern Hebei Province is located in the northern margin of the North China Craton,but magmatic genesis and tectonic setting of Neoarchean igneous rocks in the area still remain controversial.Systematic geochronologic and geochemical study of Neoarchean supracrustal and intrusive rocks in Qinglong-Shuangshanzi area,eastern Hebei are presented in this paper.Zircon LA-MC-ICP-MS U-Pb isotopic dating reveals that the meta-andesite erupted at 2 576 Ma,and the intrusive rocks(gabbro-diorites,tonalites and quartz diorites)emplaced in a range of 2 484 Ma to 2 535 Ma.Part of the early-formed meta-andesites shows high-Mg andesite geochemical characteristics,which indicates these rocks were generated from partial melting of mantle wedge peridotite metasomatised by fluids from dehydration of the subducted slab.The magnesian diorites show adakite characteristics,which suggests they have source characteristics of partial melting of mantle wedge peridotite metasomatised by felsicmelts of the subducted slab.Both of the high-Mg meta-andesites and adakite like magnesian diorites belong to a suite of island arc assemblages.Combining previous regional studies,it is concluded that Qinglong-Shuangshanzi area was under a tectonic setting of active continental margin during Neoarchean era.
Eastern Hebei Province is located in the northern margin of the North China Craton,but magmatic genesis and tectonic setting of Neoarchean igneous rocks in the area still remain controversial.Systematic geochronologic and geochemical study of Neoarchean supracrustal and intrusive rocks in Qinglong-Shuangshanzi area,eastern Hebei are presented in this paper.Zircon LA-MC-ICP-MS U-Pb isotopic dating reveals that the meta-andesite erupted at 2 576 Ma,and the intrusive rocks(gabbro-diorites,tonalites and quartz diorites)emplaced in a range of 2 484 Ma to 2 535 Ma.Part of the early-formed meta-andesites shows high-Mg andesite geochemical characteristics,which indicates these rocks were generated from partial melting of mantle wedge peridotite metasomatised by fluids from dehydration of the subducted slab.The magnesian diorites show adakite characteristics,which suggests they have source characteristics of partial melting of mantle wedge peridotite metasomatised by felsicmelts of the subducted slab.Both of the high-Mg meta-andesites and adakite like magnesian diorites belong to a suite of island arc assemblages.Combining previous regional studies,it is concluded that Qinglong-Shuangshanzi area was under a tectonic setting of active continental margin during Neoarchean era.
引文
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Martin,H.,1999.Adakitic Magmas:Modern Analogues of Archaean Granitoids.Lithos,46(3):411-429.https://doi.org/10.1016/s0024-4937(98)00076-0
Martin,H.,Moyen,J.F.,Rapp,R.,2009.The Sanukitoid Series:Magmatism at the Archaean-Proterozoic Transition.Earth and Environmental Science Transactions of the Royal Society of Edinburgh,100(1-2):15-33.https://doi.org/10.1017/s1755691009016120
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Sun,H.Y.,Dong,C.Y.,Xie,H.Q.,et al.,2010.The Formation Age of the Neoarchean Zhuzhangzi and Dantazi Groups in the Qinglong Area,Eastern Hebei Province:Evidence from SHRIMP U-Pb Zircon Dating.Geological Review,56(6):888-898(in Chinese with English abstract).
Tatsumi,Y.,2008.Making Continental Crust:The Sanukitoid Connection.Chinese Science Bulletin,53(11):1620-1633.https://doi.org/10.1007/s11434-008-0185-9
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Defant,M.J.,Drummond,M.S.,1990.Derivation of Some Modern Arc Magmas by Melting of Young Subducted Lithosphere.Nature,347(6294):662-665.https://doi.org/10.1038/347662a0
Deng,J.F.,Liu,C.,Feng,Y.F.,et al.,2010.High Magnesian Andesitic/Dioritic Rocks(HMA)and Magnesian Andesitic/Dioritic Rocks(MA):Two Igneous Rock Types Related to Oceanic Subduction.Geology in China,37(4):1112-1118.(in Chinese with English abstract).
Fu,J.H.,Liu,S.W.,Chen,X.,et al.,2016.Petrogenesis of Taxitic Dioritic-Tonalitic Gneisses and Neoarchean Crustal Growth in Eastern Hebei,North China Craton.Precambrian Research,284:64-87.https://doi.org/10.1016/j.precamres.2016.08.002
Fu,J.H.,Liu,S.W.,Wang,M.J.,et al.,2017.Late Neoarchean Monzogranitic-Syenogranitic Gneisses in the Eastern Hebei-Western Liaoning Province,North China Craton:Petrogenesis and Implications for Tectonic Setting.Precambrian Research,303:392-413.https://doi.org/10.1016/j.precamres.2017.05.002
Geng,Y.S.,Liu,F.L.,Yang,C.H.,et al.,2006.Magmatic Event at the End of the Archean in Eastern Hebei Province and Its Geological Implication.Acta Geologica Sinica,80(12):187-187(in Chinese with English abstract).
Guo,R.R.,Liu,S.W.,Bai,X.,et al.,2014.Geochemistry and Zircon U-Pb Chronology of Shuangshanzi Group in the Eastern Hebei Province,North China Craton:Constraints on Petrogenesis and Tectonic Setting.Acta Petrologica Sinica,30(10):2885-2904(in Chinese with English abstract).
Guo,R.R.,Liu,S.W.,Bai,X.,et al.,2017.A Neoarchean Subduction Recorded by the Eastern Hebei Precambrian Basement,North China Craton:Geochemical Fingerprints from Metavolcanic Rocks of the SaheqiaoShangying-Qinglong Supracrustal Belt.Journal of Asian Earth Sciences,135:347-369.https://doi.org/10.1016/j.jseaes.2017.01.007
Guo,R.R.,Liu,S.W.,Santosh,M.,et al.,2013.Geochemistry,Zircon U-Pb Geochronology and Lu-Hf Isotopes of Metavolcanics from Eastern Hebei Reveal Neoarchean Subduction Tectonics in the North China Craton.Gondwana Research,24(2):664-686.https://doi.org/10.1016/j.gr.2012.12.025
Guo,R.R.,Liu,S.W.,Wyman,D.,et al.,2015.Neoarchean Subduction:A Case Study of Arc Volcanic Rocks in QinglongZhuzhangzi Area of the Eastern Hebei Province,North China Craton.Precambrian Research,264:36-62.https://doi.org/10.1016/j.precamres.2015.04.007
Guo,S.F.,Hou,J.L.,Pan,W.,et al.,2008.Discussion on Several Problems of Qinglong River Depression Belt in Eastern Hebei Province.Hebei Geology,(3):4-7(in Chinese).
Jolly,W.T.,Schellekens,J.H.,Dickin,A.P.,2007.High-Mg Andesites and Related Lavas from Southwest Puerto Rico(Greater Antilles Island Arc):Petrogenetic Links with Emplacement of the Late Cretaceous Caribbean Mantle Plume.Lithos,98(1-4):1-26.https://doi.org/10.1016/j.lithos.2007.01.011
Kay,R.W.,1978.Aleutian Magnesian Andesites:Melts from Subducted Pacific Ocean Crust.JournalofVolcanology andGeothermalResearch,4(1-2):117-132.https://doi.org/10.1016/0377-0273(78)90032-x
Lin,Q.,Liu,S.W.,1991.Metamorphic Texture,P-T-t Path and Water Activies of Tonalitic Gneisses in Eastern Hebei Province.Journal of Jiling University(Earth Science Edition),21(3):269-276,300(in Chinese with English abstract).
Liu,B.R.,Neubauer,F.,Liu,J.L.,et al.,2017.Neoarchean Ductile Deformation of the Northeastern North China Craton:The Shuangshanzi Ductile Shear Zone in Qinglong,Eastern Hebei,North China.Journal of Asian Earth Sciences,139:224-236.https://doi.org/10.1016/j.jseaes.2017.01.014
Liu,C.H.,Zhao,G.C.,Liu,F.L.,et al.,2014.Zircon U-Pb and LuHf Isotopic and Whole-Rock Geochemical Constraints on the Provenance and Age of the Shuangshanzi and Qinglonghe Groups in Eastern Hebei:Implications for the Tectonic Evolution of the Eastern Block.Precambrian Research,255:699-715.https://doi.org/10.1016/j.precamres.2014.05.016
Liu,S.W.,Wang,W.,Bai,X.,et al.,2018.Lithological Assemblages of Archean Meta-Igneous Rocks in Eastern Hebei-Western Liaoning Provinces of North China Craton,and Their Geodynamic Implications.Earth Science,43(1):44-56(in Chinese with English abstract).
Lu,J.S.,Zhai,M.G.,Lu,L.S.,et al.,2017.P-T-t Evolution of Neoarchaean to Paleoproterozoic Pelitic Granulites from the Jidong Terrane,Eastern North China Craton.Precambrian Research,290:1-15.https://doi.org/10.1016/j.precamres.2016.12.012
Lü,B.,Zhai,M.G.,Li,T.S.,et al.,2012.Zircon U-Pb Ages and Geochemistry of the Qinglong Volcano-Sedimentary Rock Series in Eastern Hebei:Implication for?2 500Ma IntraContinental Rifting in the North China Craton.Precambrian Research,208-211:145-160.https://doi.org/10.1016/j.precamres.2012.04.002
Martin,H.,1999.Adakitic Magmas:Modern Analogues of Archaean Granitoids.Lithos,46(3):411-429.https://doi.org/10.1016/s0024-4937(98)00076-0
Martin,H.,Moyen,J.F.,Rapp,R.,2009.The Sanukitoid Series:Magmatism at the Archaean-Proterozoic Transition.Earth and Environmental Science Transactions of the Royal Society of Edinburgh,100(1-2):15-33.https://doi.org/10.1017/s1755691009016120
Middlemost,E.A.K.,1994.Naming Materials in the Magma/igneous Rock System.Earth-Science Reviews,37(3/4):215-224.https://doi.org/10.1016/0012-8252(94)90029-9
Nutman,A.P.,Wan,Y.S.,Du,L.L.,et al.,2011.Multistage Late Neoarchaean Crustal Evolution of the North China Craton,Eastern Hebei.Precambrian Research,189(1-2):43-65.https://doi.org/10.1016/j.precamres.2011.04.005
Qi,H.L.,Hao,X.H.,Zhang,X.D.,et al.,1999.The Geological Features of Granite Greenstone Belts in Qinglong River,Jidong.Progress in Precambrian Research,22(4):1-17(in Chinese with English abstract).
Shen,B.F.,Yang,C.L.,Li,J.J.,et al.,2005.New Evidence for Dating the Zhuzhangzi Group of Eastern Hebei.Journal of Stratigraphy,29(Suppl.1):433-436.(in Chinese with English abstract).
Sun,H.Y.,Dong,C.Y.,Xie,H.Q.,et al.,2010.The Formation Age of the Neoarchean Zhuzhangzi and Dantazi Groups in the Qinglong Area,Eastern Hebei Province:Evidence from SHRIMP U-Pb Zircon Dating.Geological Review,56(6):888-898(in Chinese with English abstract).
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