康古尔塔格缝合带的变形机制  

DEFORMATION FEATURE OF THE KUNGGARTAG COLLISION BELT, EAST OF NORTH TIANSHAN

作　　者：王洋[1] 陈练武[1] 

机构地区：[1]西安地质学院院长办公室,西安矿业学院

出　　处：《西安地质学院学报》1996年第4期33-38,共6页

摘　　要：北天山东段康古尔塔格带是晚古生代塔里木板块和准噶尔板块碰撞的结果。它是一条复杂的、强烈的高应变带．并具有独特的变形机制、应变序列以及构造变形。本文运用构造－地层研究方法对该碰撞带的构造特征加以分析和研究。The Kunggartag belt, which has been discovered to be a complicate high--strain belt with its own deformation mechanism and strain succession, is a late Palaeozic era collision tectonic one of the Tarim plate withthe Zhuunger plate. In this paper, the deformation feature of the belt is analysed and studied with the tectonostratigraphical division.

关 键 词：北天山 康古尔塔格带 构造层次 构造变形 

分 类 号：P551[天文地球—构造地质学]