Paleokarstic water tables and their control on reservoirs in Ordovician Yingshan Formation, Tazhong Area, Tarim Basin, NW China |
Haizhou QU,Maoyao LIU,Yunfeng ZHANG,Zhenyu WANG,Zhenghong ZHANG,Shiyin LI,Xingliang DENG |
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Fig. 5. Characteristics of karst fabrics in horizontal underflow zone below first-stage water table in different karst paleogeomorphic units. (a), (b) Cystic dissolved vugs and near horizontal dissolved fractures in first-stage horizontal underflow zone in karst highland, the former accounting for about 75% of the total thickness of karst fabrics; (c), (d) Cystic dissolved vugs and near horizontal dissolved fractures in first-stage horizontal underflow zone in karst slope, the former accounting for about 63% of the total thickness of karst fabrics; (e), (f) Near horizontal dissolved fractures and cystic dissolved vugs in first-stage horizontal underflow zone in karst depression, the former making up about 58% of the total thickness of karst fabrics. |