塔里木盆地西部及邻区构造格局与演化  

TECTONIC FRAMEWORK AND EVOLUTION OF WESTERN TARIM BASIN AND NEIGHBORING AREAS

作　　者：成守德[1] 刘朝荣[2] 肖立新[2] 

机构地区：[1]新疆维吾尔自治区地质矿产勘查开发局地质矿产研究所,新疆乌鲁木齐830000 [2]中国石油新疆油田分公司勘探开发研究院地球物理研究所,新疆乌鲁木齐830011

出　　处：《新疆地质》2002年第z1期13-18,共6页Xinjiang Geology

基　　金：国家95重点科技攻关项目(961110310)资助

摘　　要：论述了塔里木盆地西部及邻区大地构造格局、沉积盆地、沉积建造及沉积地层层序及主要地质事件.将区域构造发展演化史概括为:古陆核的形成,原始古陆的发展,古亚洲洋的产生与封闭,特提斯洋的形成、发展与消亡4大阶段.The principle is described on division of tectonic units. Tectonic divisions have been made for areas including western Tarim basin and neighboring Pamir plateau, southwestern Tianshan mountains and Karakum basin. They are, from north to south, Kazakhstan-Junggar block, Karakum-Tarim block; South China block (Yangse block), Tibet-Yunnan intermediate block and India block, bounded by Central Tianshan suture, Kangxiwar-East Kunlun central fault, Pamir northern margin-Kangxiwa-Dahongliutan-Jinshajiang suture and Kohistan-Ladahk-Yarlung Zangbo suture. Descriptions are given on major sedimentary basins, sedimentary formation and sequence as well as geological events. The regional tectonic development is generalized as four stages, i.e., formation of old continent, development of proto-continent, formation and closure of paleo-Asian ocean, and development and closure of Tethyan oceans.

关 键 词：塔里木盆地 帕米尔高原 西南天山 卡拉库姆盆地 构造格局 

分 类 号：P544[天文地球—构造地质学]