西北地质2017，Vol.50Issue(3)：126-139,14.
巴基斯坦及中国邻区构造单元划分及其演化
Tectonic Unit Division and Geological Evolution of Pakistan and Its Adjacent Regions
摘要
Abstract
Pakistan is located in the middle section of the Tethyan tectonic domain,where is the junction of India plate,Eurasian plate and Arabian plate,thus it serves as one of the hot spots for studying the Himalayan orogeny and Tethys tectonic domain.Based on the previous studies,the tectonic units of Pakistan and its adjacent regions has been divided,and their geological evolution has been discussed,which provide some basic data for the geosciences comparative study of the border region in China and Pakistan.This studying area has been divided into 3 first-order tectonic units (Karakurn-Tarim plate,Middle Iran-Gangdese intermediate plate and Indian plate),13 secondary tectonic units and 11 third-grade tectonic units by taking Bamiyan-Kangxiwa suture and Kohistan-Ladakh suture as the boundaries,and then the geological characteristics of these tectonic units have been introduced.Finally,the evolution of this studying area has been discussed from the formation and evolution of Paleo-and Neo-Tethys Oceans,as well as the continent-continent collision.During the evolution process of Paleo-and Neo-Tethys Oceans,South Pamir,Qiangtang and Lhasa blocks were separated from the north margin of Gondwana supercontinent,and then the Bamiyan-Kangxiwa,Kohistan-Ladakh,Yarlungzangbo sutures,Main Karakorum and Main Mantle faults were formed successively,which constitute the main tectonic framework of this studying area.During the continent-continent collision orogeny process,a series of fault systems and related rifting systems or rifting basins were formed by the crustal extension and rifting,which reconstruct the edge and shape of original sedimentary basin and control the emplacement and spatial distribution of various rocks.关键词
构造单元/地质特征/演化/巴基斯坦Key words
tectonic unit/geological characteristics/evolution/Pakistan分类
天文与地球科学引用本文复制引用
吕鹏瑞,姚文光,张辉善,孟广路,张海迪..巴基斯坦及中国邻区构造单元划分及其演化[J].西北地质,2017,50(3):126-139,14.基金项目
中国地质调查局“乌兹别克斯坦、塔吉克斯坦及邻区矿产资源潜力评价”(121201011000150010),“苏莱曼山-喀喇昆仑山成矿地质背景和成矿规律对比研究”(1212011120336)和“中亚南亚资源潜力综合分析与成果应用”(12120115066601)国际地质对比计划(ICGP/SIDA-600)联合资助 （121201011000150010）
