泰国北部晚泥盆世后碰撞岩浆岩:对特提斯演化的启示  

Late Devonian Post⁃Collisional Magmatic Rocks in Northern Thailand:Implication for the Tethyan Evolution

作　　者：刘方凯 冯庆来[1,2] 赵天宇[2] Punyawai Wunnaporn Khanmanee Jongkonnee Liu Fangkai;Feng Qinglai;Zhao Tianyu;Wunnaporn Punyawai;Jongkonnee Khanmanee(State Key Laboratory of Geological Processes and Mineral Resources,Wuhan 430074,China;Faculty of Earth Sciences,China University of Geosciences,Wuhan 430074,China;Faculty of International Education,China University of Geosciences,Wuhan 430074,China)

机构地区：[1]中国地质大学地质过程与矿产资源国家重点实验室,湖北武汉430074 [2]中国地质大学地球科学学院,湖北武汉430074 [3]中国地质大学国际教育学院,湖北武汉430074

出　　处：《地球科学》2024年第8期2736-2750,共15页Earth Science

基　　金：国家自然科学基金项目(No.41672222)。

摘　　要：东南亚特提斯构造带的研究主要集中在晚古生代古特提斯的演化,而对于原特提斯演化的研究非常薄弱.对泰国北部花岗岩和角闪辉长岩进行了锆石U-Pb年代学、地球化学及锆石Lu-Hf同位素研究.这些岩浆岩的加权平均年龄为367~361 Ma,时代为晚泥盆世.泰北花岗岩属高钾钙碱性A2型花岗岩,具备LILE相对富集,HFSE相对亏损的地球化学特征,具明显的Nb、Ta、Sr和Ti的负异常.Hf同位素具有正εHf(t)值(+5.43~+10.91),T_(DM2)年龄在1015.0~668.9 Ma之间,来源于年轻的镁铁质下地壳.角闪辉长岩具高含量的Al_(2)O_(3)、Zr和Nb,低含量的TiO_(2)、Ni,LILE相对富集和HFSE相对亏损,明显的Nb和Ta负异常,类似于岛弧钙碱性玄武岩特征.正的εHf(T)值(+1.24~+9.11)和高的Mg^(#)(50.0~64.8)表明其来源于亏损的地幔楔.根据泰国北部岩浆岩U-Pb年龄、Hf同位素及地球化学特征,认为它们形成于晚泥盆世后碰撞伸展构造背景下,可以与缅甸东部、云南西南部同期原特提斯地质记录对比,该成果为滇西南及东南亚地区原特提斯演化提供了依据.The studies of the Tethys tectonic belt in Southeast Asia mainly focus on the evolution of the Paleo-Tethys in the Late Paleozoic,while the studies of the Proto-Tethys evolution immediately are pretty weakThe present study focuses on zircon U-Pb geochronology,geochemistry and zircon Lu-Hf isotopes of granites and hornblende gabbros from northern Thailand.These magmatic rocks yielded zircon U-Pb weighted mean age of 367-361 Ma.The geologic age is the Late Devonian.The northern Thailand granites are the high-K calc-alkaline A2 type granites,with the geochemical characteristics of relatively enriched LILE and relatively depleted HFSE,with obvious negative anomalies of Nb,Ta,Sr and Ti.The Hf isotopes have positiveεHf(t)values(+5.43-+10.91)with T_(DM2) ages of 1015.0-668.9 Ma,indicating a juvenile mafic lower crust source.The hornblende gabbros showhigh Al_(2)O_(3)、Zr and Nbcontents,but low contents of TiO_(2) and Ni,with the geochemical characteristics ofrelatively enriched LILE and relatively depleted HFSE,with the distinctly negative Nb and Ta anomalies,similar to the characteristics of island arc calc-alkaline basalts.PositiveεHf(t)values(+1.24-+9.11)and high Mg^(#)(50.0-64.8)indicate that it originates from the depleted mantle wedge.Based on the U-Pb age,Hf isotope and geochemical characteristics of the magmatic rocks in northern Thailand,it is believed that they were formed in the Late Devonian post-collisional extension-related tectonic setting,which can be compared with the corresponding the Proto-Tethys geological records in eastern Myanmar and southwestern Yunnan.The results provide evidence for the evolution of the Proto-Tethys in southwest Yunnan and Southeast Asia.

关 键 词：晚泥盆世 特提斯 岩浆岩 后碰撞 泰国北部 地球化学 

分 类 号：P547[天文地球—构造地质学]