Origin and characteristics of grain dolomite of Ordovician Ma5 5 Member in the northwest of Ordos Basin, NW China |
ZHANG Xi,ZHANG Tingshan,LEI Bianjun,ZHANG Jingxuan,ZHANG Ji,ZHAO Zhongjun,YONG Jinjie |
Fig. 5. Core photographs, common slices, and Scanning Electron Microscope Photograph of dolomicrite from Well SD39-62C1. (a) 3 116.38 m, dolomicrite, birdeye structure, common slice; (b) 3 115.37 m, dolomicrite, gypsum pseudo-crystal, common slice; (c) 3 141.20 m, dolomicrite, rodlike gypsum pseudo-crystal, common slice; (d) 3 138.20 m, dolomicrite, gypsum pseudo-crystal, common slice; (e) 3107.45 m, dolomicrite, dense, Scanning Electron Microscope; (f) 3 107.45 m, dolomicrite, cathodoluminescence photograph. |