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西昆仑山—喀喇昆仑山的构造分区及其演化

THE DIVISION AND EVOLUTION OF TECTONIC AREA IN WESTERN KUNLUN MT. -KARAKORUM MT.

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【作者】 张志德曾亚参

【Author】 Zhang Zhide Zeng Yashen(No,1 Regional Geological Serveying Party, Bureau (Geological Department ofof Geology and Mineral Resources of Xinjiang) Xinjiang Engineering College)

【机构】 新疆地质矿产局第一区调大队新疆工学院地质系

【摘要】 <正> 本文研究范围为塔里木盆地西南的苦牙克断裂以西直至国界线的广大地区,包括西昆仑山和喀喇昆仑山.即东经73°—84°,北纬34°—39°.笔者运用历史构造分析并结合板块构造理论,对该区的构造区划及其演化进行了初步探讨.由于笔者水平有限,不妥之处,望批评指正.

【Abstract】 In this paper, Western Kunlun Mt.-Karakorum Mt. region is divided into three areas and seven subareas in tectonics, as follows:1. Tarim platform area( Ⅰ ), including Yenggisar-Hotan depression ( Ⅰ2), Tekilik fault uplift ( Ⅰ 2), Qarlung-Korlang intracontinental fold belt ( Ⅰ 3), Kongur-Sanju fault uplift ( Ⅰ 4).2. Karakorum fold system (Ⅱ), including Aksayqin-Qiangtang uplift belt (Ⅱ1), Bayanhar Indo-Sinian fold belt ( Ⅱ 2), Linjitang Yanshan foldbelt (Ⅱ3).3. Gangdice folde system (Ⅲ).The charateristics of tectonic evolution are also discribed for every area, It should be noted that the author takes the southern boundary of Tarim platform to the Kengxiwar great fault.

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