- 责任者：Zhao Xing (Key Laboratory of Orogenic Belts and Crustal Evolution ; School of Earth and Space Sciences ; Peking University ; Beijing 100871 ; China) ; Li Jianghai
- 刊名：Geological Journal of China Universities
- 出版年：2009
- 卷期：15(1)
- 关键词：盐构造 ; salt tectonics ; 塔里木盆地 ; Tarim Basin
- 页码：p.115-125
- 图表：11 illus., 24 refs.
- 分类号：0300
- issnNo：ISSN1006-7493
- isbnNo：CN32-1440/P
Based on seismic and well data, the salt structure styles, formation mechanism and influence on regional tectonics of Tabei Uplift is investigated in this paper in Yingmai 2 work district, Yingmaili area, western Tabei Uplift. It is implied that western Tabei Uplift underwent strike slip movement in Late Paleozoic when salt deformation took place. Salt structures were deformed in compressional tectonic setting in Late Paleozoic and, according to the analysis of the structural evolution section, the main fault was remobilized as a synsedimentary fault in Triassic with a limited scale. After Triassic these structures were relatively stable. Salt layers significantly influenced the tectonic deformation. In structural layers below and above them, inharmonious structure styles were formed.