LI Yong, HOU Ming-cai, KANG Kong-yue, ZHANG Jie, CHEN Lin. Sedimentary environments of the B Formation of the Upper Carboniferous Qiati'er Group in the Tianshuihai-Mazar block, western Kunlun Mountains[J]. Sedimentary Geology and Tethyan Geology, 2013, 33(1): 55-61.
Citation: |
LI Yong, HOU Ming-cai, KANG Kong-yue, ZHANG Jie, CHEN Lin. Sedimentary environments of the B Formation of the Upper Carboniferous Qiati'er Group in the Tianshuihai-Mazar block, western Kunlun Mountains[J]. Sedimentary Geology and Tethyan Geology, 2013, 33(1): 55-61.
|
Sedimentary environments of the B Formation of the Upper Carboniferous Qiati'er Group in the Tianshuihai-Mazar block, western Kunlun Mountains
-
1. State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Chengdu University of Technology, Chengdu 610059, Sichuan, China;
2. Institute of Sedimentary Geology, Chengdu University of Technology, Chengdu 610059, Sichuan, China;
3. No. 282 Geological Party, Sichuan Geological Bureau of Nuclear Industry, Deyang 618200, Sichuan, China
-
Abstract
The petrographic associations and sedimentary environments are treated for the B Formation of the Upper Carboniferous Qiati'er Group in the Tianshuihai-Mazar block, western Kunlun Mountains in terms of sedimentary structures, thin section and grain-size analysis. The lithology in the Formation consists of fine-grained sandstone, siltstone, mudstone and shale, which are involved into a succession of lacustrine-continental delta deposits. The delta facies may be subdivided into the delta plain, delta front and prodelta subfacies. The detritus come from the recycled orogen and mixed source areas. The results of research in this study will provide important information for better understanding of the tectonic evolution of western Qinghai-Xizang Plateau.
-
-
-
Access History