川西雀儿山花岗杂岩体锆石U-Pb年龄、地球化学特征及其成矿专属性
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摘要
川西义敦岛弧碰撞造山带北段雀儿山复式花岗杂岩体的年代学和全岩地球化学研究表明,雀儿山杂岩体主要由花岗闪长岩、二长花岗岩和正长花岗岩组成。锆石LA--ICP--MS U--Pb测年结果显示,该岩体中的花岗闪长岩形成时代为晚三叠世(224±3 Ma),二长花岗岩则形成于早白垩世(102±1 Ma)。地球化学数据表明,晚三叠世花岗闪长岩为火山弧岩石序列,形成环境为碰撞前俯冲环境;早白垩世二长花岗岩和正长花岗岩为后碰撞岩石序列,形成于造山期后板内或陆内环境。结合区域地质资料,认为雀儿山杂岩体为印支期—燕山期义敦岛弧碰撞造山带经历俯冲--碰撞--隆升过程中的产物。
The study of geochronology and whole-rock geochemistry in Que'ershan granitic complex from the northern Yidun arc collision-orogenic belt,western Sichuan shows that Que'ershan complex consists mainly of granodiorite,monzogranite and syenogranite.The results of zircon LA--ICP--MS U--Pb data indicate that the granodioriteof this granitic complex formed in the Late Triassic(224 ± 3 Ma),and the monzogranite was emplaced in the Early Cretaceous(102 ± 1 Ma).The geochemical data suggest that the Late Triassic granodiorites belong to the volcanic arc granite series,and might form in a pre-collision subduction setting,whereas the Early Cretaceous monzogranites and syenogranites belong to post-collisional rock serious,and probably formed within plate or continent during the post-orogeny stage.In combination with regional geological data,the authors propose that the Que'ershan granitic complex were results of subduction-collision-uplift of Yidun arc collision-orogenic belt during Indosinian-Yanshanian period.
The study of geochronology and whole-rock geochemistry in Que'ershan granitic complex from the northern Yidun arc collision-orogenic belt,western Sichuan shows that Que'ershan complex consists mainly of granodiorite,monzogranite and syenogranite.The results of zircon LA--ICP--MS U--Pb data indicate that the granodioriteof this granitic complex formed in the Late Triassic(224 ± 3 Ma),and the monzogranite was emplaced in the Early Cretaceous(102 ± 1 Ma).The geochemical data suggest that the Late Triassic granodiorites belong to the volcanic arc granite series,and might form in a pre-collision subduction setting,whereas the Early Cretaceous monzogranites and syenogranites belong to post-collisional rock serious,and probably formed within plate or continent during the post-orogeny stage.In combination with regional geological data,the authors propose that the Que'ershan granitic complex were results of subduction-collision-uplift of Yidun arc collision-orogenic belt during Indosinian-Yanshanian period.
引文
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[7]王全伟,王康明,阚泽忠,等.川西地区花岗岩及其成矿系列[M].北京:地质出版社,2008:1-305.WANG Quan-wei,WANG Kang-ming,KAN Ze-zhong,et al.Granitoids and mineralization series western Sichuan Province[M].Beijing:Geological Publishing House,2008:1-305.
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[9]Andersen T.Correction of common lead in the U--Pb analyses that do not report204Pb[J].Chemical Geology,2012,192(1/2):59-79.
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[13]Maniar P D,Piecoli P M.Tectonic discrimination of granitoids[J].Geological Society of American Bulletin,1989,101(5):635-643.
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[15]Boynton W V.Geochemistry of the rare earth elements:meteorite studies[C]//Henderson P.Rare Earth Elements Geochemistry,Elsevier,Amsterdam,1984:63-114.
[16]Sun W D,Mc Donough W F.Chemical and isotopic systematics of oceanic basalts:implications for mantle composition and processes[J].Geological Society,London,Special Publications,1989,42(1):313-345.
[17]蒲建彬,张兴洲,郭冶,等.佳木斯地块东部二叠纪方山花岗岩体的锆石U--Pb年代学、地球化学特征及其地质意义[J].世界地质,2015,34(4):903-913.PU Jian-bin,ZHANG Xing-zhou,GUO Ye,et al.Geological implications of Permian Fangshan granitic rocks in eastern Jiamusi Massif:evidences from U--Pb chronology and geochemistry[J].Global Geology,2015,34(4):903-913.
[18]吴福元,李献华,杨进辉,等.花岗岩成因研究的若干问题[J].岩石学报,2007,23(6):1217-1238.WU Fu-yuan,LI Xian-hua,YANG Jin-hui,et al.Discussions on the petrogenesis of granites[J].Acta Petrologica Sinica,2007,23(6):1217-1238.
[19]李小伟,莫宣学,赵志丹,等.关于A型花岗岩判别过程中若干问题的讨论[J].地质通报,2010,29(2/3):278-285.LI Xiao-wei,MO Xuan-xue,ZHAO Zhi-dan,et al.A discussion on how to discriminate A-type granite[J].Geological Bulletin of China,2010,29(2/3):278-285.
[20]张旗.A型花岗岩的标志和判别:兼答汪洋等对“A型花岗岩的实质是什么”的质疑[J].岩石矿物学杂志,2013,32(2):267-174.ZHANG Qi.The criteria and discrimination for A-type granites:a reply to the question put forward by Wang Yang and some other persons for“A-type granite:what is the essence?”[J].Acta Petrologica et Mineralogica,2013,32(2):267-174.
[21]纪政,葛文春,杨浩,等.大兴安岭中段塔尔气地区早白垩世花岗岩成因及形成构造环境[J].世界地质,2016,35(2):283-296.JI Zheng,GE Wen-chun,YANG Hao,et al.Petrogenesis of Early Cretaceous granites in Taerqi area of central Great Xing'an range and its tectonic setting[J].Global Geology,2016,35(2):283-296.
[22]马国祥,王之晟,郝晓飞,等.阿尔山地区金江沟高分异I型花岗岩锆石U--Pb年龄、岩石地球化学及构造意义[J].世界地质,2016,35(1):89-98.MA Guo-xiang,WANG Zhi-sheng,HAO Xiao-fei,et al.U--Pb dating,geochemistry and geological setting of I-type granite in Jinjianggou,Arshan area[J].Global Geology,2016,35(1):89-98.
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[26]Watson E B,Harrison T M.Zircon saturation revisited:temperature and composition effects in a variety of crustal magma types[J].Earth and Planetary Science Letters,1983,64(2):295-304.
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