Tectonic paleogeography of Late Sinian and its significances for petroleum exploration in the middle-upper Yangtze region, South China |
WANG Zecheng,JIANG Hua,CHEN Zhiyong,LIU Jingjiang,MA Kui,LI Wenzheng,XIE Wuren,JIANG Qingchun,ZHAI Xiufen,SHI Shuyuan,LI Qi |
Fig. 5. Typical petrological characteristics of the Dengying Formation in the middle and upper Yangtze region. (A) Evaporative lagoon, dolomite containing gypsum clumps (Well Wei 117, Deng 1 Member); (b) restricted platform, barite-bearing micritic dolomite (Huize Yinchangpo section, Deng 2 Member); (c ) Restricted platform, siliceous band dolomite (E’bian Xianfeng section, Deng 4 Member); (d) Platform margin, dolarenite (Well Moxi 108, Deng 4 Member); (e) Intra-platform dolomite with algal layers (Xianfeng section of E’bian, Deng 2 Member); (f) micritic dolomite at platform margin (Gaoshi 102, Deng 4 Member); (g) dolarenite inside platform (Well Zitan 1, Deng 2 Member); (h) thin micritic dolomite in platform sag (Yangjiaping section of Shimen, Deng 1 Member); (i) restricted platform, dolomite with algal laminae (Well Moxi 108, Deng 2 Member); (j) platform margin slope, dolomite and layered siliceous dolomite (Zhenba Laoqihe section, Deng 4 Member). |