Characteristics of parametamorphic rock reservoirs in Pingxi area, Qaidam Basin, NW China |
Zhiyuan XIA,Zhanguo LIU,Senming LI,Yongshu ZHANG,Bo WANG,Mingzhi TIAN,Jin WU,Kaizhen ZOU |
Fig. 4. Pore characteristics of three kinds of parametamorphic rock reservoirs in Pingxi area. (a) Well Dp172, 4 405 m, Silurian, slate, rich in dissolution microspores, micro-CT photograph; (b) Well Dp17, 4 397 m, Ordovician, crystalline limestone, dissolved pores along structural fractures, micro-CT photograph; (c) Well Dp172, 4 599 m, Ordovician, calc-schist, dissolution pores along cleavages, micro-CT photograph. |