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准噶尔板块东北缘富铌玄武岩的发现及其地质意义

DISCOVERY OF Nb-RICH BASALT AT THE NORTHEAST MARGIN OF JUNGGAR PLATE AND THE GEOLOGICAL SIGIFICANCE

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【作者】 张海祥牛贺才于学元单强Hiroaki SatoJunichi Ito

【Author】 ZHANG Haiyang1, NIU Hecai1, YU Xueyuan1, SHAN Qiang1, Hiroaki Sato2, Junichi Ito2(1.Guangzhou Geochemical Institute of the Chinese Academy of Sciences, Guangzhou 510640, China;2.Department of Earth and Planetary Sciences, Faculty of Science, Kobe University, Kobe 6578501, Japan)

【机构】 中国科学院广州地球化学研究所日本神户大学理学部地球惑星科学教室日本神户大学理学部地球惑星科学教室 广东广州510640广东广州510640神户657-8501神户657-8501

【Abstract】 Nbrich basalt is discovered for the first time in uoranggekuduke formation of Lower carboniferous series, Fuyun county in the Northeast margin of Junnggar plate. It is derived from depth of 70~100 km and formed by partial melted peridodite of the mantle wedge which was replaced by adakite melting material, and is the product of the subduction of the palacoAsia ocean plate. The discovery implies a south subduction of the palaeoAsia oceanic crust toward Junggar plate during Early Carboniferous Epoch.

【基金】 国家自然科学基金(编号:400073006);973项目(编号:2001CB409805)联合资助。
  • 【文献出处】 地质找矿论丛 ,Contributions To Geology and Mineral Resources Research , 编辑部邮箱 ,2003年01期
  • 【分类号】P588.1
  • 【被引频次】23
  • 【下载频次】228
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