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阿尔金断裂两侧构造单元的对比及岩石圈剪切机制
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Cite This Paper:.1999.A Comparison between the Tectonic Units on the Two Sides of the Altun Sinistral Strike-slip Fault and the Mechanism of Lithospheric Shearing[J].Acta Geologica Sinica,73(3):
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许志琴  杨经绥
中国地质科学院地质研究所,中国地质科学院地质研究所,中国地质科学院地质研究所,中国地质科学院地质研究所,中国地质科学院地质研究所,中国地质科学院地质研究所 北京,100037,北京,100037,北京,100037,北京,100037,北京,100037,北京,100037
基金项目:地质矿产部“九五”重点基础项目(编号9501106),国家自然科学基金(编号49732027),国家“973”项目成果
中文摘要:中亚最大在阿尔金走滑断裂系统成了青藏高原的北部边界,阿尔金北缘断裂及阿尔金左行瞳滑断裂(阿尔金主断裂)所夹持的阿尔金地体自北往南由敦煌地块、北阿尔金加里东俯冲杂岩带、中阿尔金地块及南阿尔金加里东俯冲-碰撞杂岩带组成,研究表明这些单元分别可与阿尔金主断裂带东侧的阿拉善地块、北祁连俯冲杂岩带、中-南祁连地块及柴达木北缘加里东俯冲-碰撞杂岩带相对比。特别通过南阿尔金与柴达木北缘榴辉石带的详细对比,发现它
中文关键词:断层 阿尔金断裂 构造单元对比 岩石圈剪切断裂
 
A Comparison between the Tectonic Units on the Two Sides of the Altun Sinistral Strike-slip Fault and the Mechanism of Lithospheric Shearing
Xu Zhiqin  Yang Jingsui  Zhang Jianxin  Jiang Mei  Li Haibing  Cui Junwen
keywords:sinistral strike-slip,subduction-collision complex,comparison between tectonic units,lithospheric shearing fault,intracontinental subduction,
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