ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
藏北多龙矿集区尕尔勤枕状玄武岩地球化学及SHRIMP测年
  
关键词:SHRIMP dating  petrogeochemistry  pllow basalt  Duolong  Tibet
基金项目:国土资源部公益性行业科研专项(编号: 201511017);自然科学基金项目(编号: 41402178);中国地质科学院院基本科研业务费(编号: YYWF201608);中国地质调查局二级项目(编号: DD20160026);中国地质调查局中国矿产地质与成矿规律综合集成和服务(矿产地质志)项目(编号: DD20160346);国家留学基金委项目
作者单位E-mail
林彬 中国地质科学院矿产资源研究所, 国土资源部成矿作用与资源评价重点实验室
澳大利亚塔斯马尼亚大学卓越矿床研究中心 
linbinlxt@sina.com 
唐菊兴 中国地质科学院矿产资源研究所, 国土资源部成矿作用与资源评价重点实验室  
宋扬 中国地质科学院矿产资源研究所, 国土资源部成矿作用与资源评价重点实验室 songyang100@126.com 
王勤 成都理工大学  
曹华文 成都地调中心  
Michael BAKER 澳大利亚塔斯马尼亚大学卓越矿床研究中心  
张乐骏 澳大利亚塔斯马尼亚大学卓越矿床研究中心  
李玉彬 西藏地质调查研究院  
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摘要:
Petrogeochemistry and SHRIMP Dating of Ga’erqin Pillow Basalt in Duolong, Northern Tibet
      Duolong is one of the largest porphyry Cu (Au) ore concentration areas, its dynamic history always being the hot topic for study. Pillow basalt was discovered in Jurassic marine sedimentary strata of Ga’erqin area. Geochronological and geochemical study is helpful to revealing the evolution history of Bangong Co-Nujiang Ocean. Geochemical data show that basalt has low REE (∑REE 38.01×10–6~63.56×10–6) and no significant differentiation between LREE and HREE. The chondrite-normalized REE patterns are flat, similar to features of E-MORB. SHRIMP dating shows that the age of pillow basalt is (298±11) Ma, coinciding with ages of mafic dykes and basalt in Late Carboniferous to Early Permian strata. All of these phenomena may be the products of large-scale volcanic activity for the opening of Bannu Ocean in early Permian strata.
LIN Bin,TANG Ju-xing,SONG Yang,WANG Qin,CAO Hua-wen,Michael BAKER,ZHANG Le-jun,LI Yu-bin.2017.Petrogeochemistry and SHRIMP Dating of Ga’erqin Pillow Basalt in Duolong, Northern Tibet[J].Acta Geoscientica Sinica,38(5):702-710.
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