天山-西昆仑地区沉积-构造演化史--新疆地学断面走廊域及邻区不同地体的沉积-构造演化

doi:10.7605/gdlxb.2001.03.002

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Abstract

Based on the researches in the "Xinjiang Geotransect" project, the sedimentary-tectonic evolutionary history of the Tianshan-Tarim-Kunlun Mts. area in Southern Xinjiang was discussed in this paper. Here, the discussion is predominant in the history of Paleozoic and Meso-Cenozoic. About the history of the crustal evolution in the study area, four periods can be divided. Generally speaking, it is the process that the paleo-oceanic basin in different periods gradually closed, the different continental plates collised and amalgamated, took the crust of this area to become more stability. The main factors for the evolution in Paleozoic were the activities of the paleo-Asian oceanic basin. By the end of Paleozoic, the paleo-Eurasian continent formed on the north part of the corridor. The evolution in Late Paleozoic to Mesozoic is controlled by the activities of the Paleo-Tethys oceanic basin in the south. Following the closing of the Tethys ocean and the collisions of the continental blocks in the south, a series of sedimentary and tectonic events took place in this area, including the closing of the paleo-Tethys oceanic basin, the forming of the Kangxiwar suture zone and some responses by the collision of Qiangtang, Gangdise and Himalayan blocks in the south. All of these formed the recent features of basin-mountain tectonics and plenty mineral resources.

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Published: 01 June 2001

About author: Liu Xun, Male; born in 1939, took postgraduate course in the Geological College of Beijing in 1965. Now he is the research fellow of the Institute of Geology, Chinese Academy of Geological Sciences, and has been engaged in the study of regional geology, tectonics and analysis of sedimentary basins for a long time. Address: Institute of Geology, Chinese Academy of Geological Sciences, 26#, Baiwanzhuang Road, Beijing. 100037.

Cite this article:

. THE HISTORY OF SEDIMENTARY - TECTONIC EVOLUTION OF THE TIANSHAN TO WEST KUNLUNAREA,WEST CHINA--the Sedimentary-Tectonic Evolution of the Terranes in the Corridor of the Xinjiang Geotransect and its Adjacent Areas[J]. JOURNAL OF PALAEOGEOGRAPHY, 2001, 3(3): 21-31.

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http://journal09.magtechjournal.com/gdlxb/EN/10.7605/gdlxb.2001.03.002 OR http://journal09.magtechjournal.com/gdlxb/EN/Y2001/V3/I3/21

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