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地球学报  2001 

新疆地学断面(独山子—泉水沟)走廓域及邻区地球物理调查综合研究

Keywords: 新疆地学断面,西昆仑,天山,塔里木,地球物理综合研究

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Abstract:

沿新疆地学断面(独山子-泉水沟)走廊域实施了多种地球物理方法调查研究。对岩石圈现今活动性、位场异常图像处理与岩石圈变形踪迹、地体基底构造与边界断裂划分等进行了综合研究。整条地学断面处于近SN向的挤压环境中。挤压力一方面来自印度板块向北的推挤,另一方面来自增厚岩石圈根带下沉的拖力。塔里木岩石圈呈刚性,且整体变形,对应力的传播起到放大的作用。阿尔金断裂向南延展进入西昆仑造山带,南端与泉水沟断裂相接,并且斜截了库地断裂和康西瓦断裂。中天山地体与北天山地体与准噶尔盆地统属同一基底构造区,南天山地体与北塔里木统属同一基底构造区。南北塔里木是2个基底性质不同的地体。40°N是分割南北塔里木的地体边界断裂。研究结果表明,新疆新构造运动不是古板块的简单复活。

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