ning: 18.0pt; mso-bidi-font-weight: bold" lang=EN-US>The Structural Styles of Different Structural Layers in the Western Part of North Tarim Uplift and Their Genetic Mechanisms
详细信息
- 责任者：Cheng Haiyan (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(4)
- 关键词：构造层 ; tectonic layer ; 构造样式 ; tectonic style ; 塔里木盆地 ; Tarim Basin
- 页码：p.529-536
- 图表：9 illus., 1 table, 23 refs.
- 分类号：0300
- issnNo：ISSN1006-7493
- isbnNo：CN32-1440/P
摘要
The Western part of North Tarim Uplift underwent several phases of tectonic evolution. Three structural layers were formed including Sinian-Paleozoic, Mesozoic-Paleogene and Neogene-Quaternary structural layers. The thrust faults, folds, strike-slip faults and magmatic diapir structures were formed in the lower layer, the negative inversion and normal faults were developed in the middle layer, while in the upper layer, the thrust faults were developed in the Yingmaili region, and the negative inversion structures were developed in the Yaha region continuously. The relations of the structures of different layers are diverse in different places. The structures of the middle and upper layers inherited those in the lower layer in the Yaha region.