塔里木盆地北部北西向断裂的特征及地球动力学机制
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THE CHARACTERISTICS oF NW—TRENDING FAULTS AND THEIR GEoDYNAMIC MECHANISM IN THE NoRTHERN TARIM BASlN
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    摘要:

    塔里木盆地北部(简称塔北)区域构造上最显著的特征是受走向ENE和 Nw两组区域性大断裂的控制,形成了南北分带、东西分块的基本构造格局n]。 本区Nw向断裂以基底卷入型压性逆冲为基本特点。构造发育受中新生代塔里 木板块西南缘大地构造演化控制。这一时期的主要地质事件有早二叠纪末期塔 里木板块与西昆仑地体的碰撞;侏罗纪西昆仑地体与喀喇昆仑地体的碰撞;第 三纪印度板块与欧亚板块的碰撞。

    Abstract:

    The most striking tectonic feature of the northem part of the Tarim basin is that it is cut by the ENE—trending regional faults,forming a tectonic franework of north—south zoning and east- west regionalization.Based on the analysis of geometry and kinematics,the author think that the main fauks striking NW in Northem Tarim Basin are Characterized by deformation of based— mentinvolved Compressional thrust,Which were controled by plate tectonics evolution of nouth- westem margin of Tarim plate during Mezo—Cenozoic time period。The most important events happened in this period were collision between western kunlun terrane and Tarim plate in the ending of early Permian,collision between Kalakunlun terrane and western Kunlun in Jurasic, and collision of Indian plate and south Asian continental margin in Tertiar

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严俊君.1996.塔里木盆地北部北西向断裂的特征及地球动力学机制[J].地质论评,42(sup):116-123,[DOI].
yan junjun.1996. THE CHARACTERISTICS oF NW—TRENDING FAULTS AND THEIR GEoDYNAMIC MECHANISM IN THE NoRTHERN TARIM BASlN[J]. Geological Review,42(sup):116-123.

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