Geological characteristics and development potential of transitional shale gas in the east margin of the Ordos Basin, NW China |
KUANG Lichun,DONG Dazhong,HE Wenyuan,WEN Shengming,SUN Shasha,LI Shuxin,QIU Zhen,LIAO Xinwei,LI Yong,WU Jin,ZHANG Leifu,SHI Zhensheng,GUO Wen,ZHANG Surong |
Fig. 4. Sedimentary characteristics of the Shan23 sub-member in Well Daji 51, Daning-Jixian area in the east margin of the Ordos Basin. (a) Core image of black organic-rich shale with foliations, 2286 m; (b) core image of carbonate bioclastic shale, 2270 m; (c) core image of silty shale with siltstone, 2261 m; (d) thin section image of shale of tidal flat-lagoon facies in deep-water still reduction environment, plane polarized light, 2295 m; (e) thin section image of shale with sideritization of charcoal debris, indicating reducing environment, plane polarized light, 2282 m; (f) thin section image of silty shale with plant debris, plane polarized light, 2261 m. |