Distribution and gas-bearing properties of Permian igneous rocks in Sichuan Basin, SW China |
MA Xinhua,LI Guohui,YING Danlin,ZHAGN Benjian,LI Ya,DAI Xin,FAN Yi,ZENG Yunxian |
Fig. 9. Images of reservoir space in Upper Permian igneous rocks of Sichuan Basin. (a) Well ZG2, 3 193.09 m, epidote basalt, dissolution pore, blue cast thin section; (b) Well ZG2, 3 026 m, porphyry basalt, dissolution pore, blue cast thin section; (c) Well ZG1, 2 988 m, porphyry basalt, primary pore, orthogonal light; (d) Well ZG2, 3 026 m, porphyry basalt, dissolution pore, blue cast thin section; (e) Well YT1, 5 647.11 m, tuff, dissolution pore, blue cast thin section; (f) Well YT1, 5 646.90 m, tuff, de-vitrification micropore, blue cast thin section; (g) Well YT1, 5 647.11 m, tuff-bearing volcanic breccia, de-vitrification micropore, blue cast thin section; (h) Well YT1, 5 645.75 m, volcanic breccia, inter-gravelly pore, (-); (i) Well YT1, 5 645.76-5 645.98 m, volcanic breccia, dissolution pore; (j) Well YT1, 6 418.13- 6426.13 m, tuffaceous volcanic breccia, dissolution pore; (k) Well ZG2, 3 181.86 m, porphyry basalt, dissolution fracture, blue cast thin section; (l) Well ZG2, 3 226.26-3 226.35 m, cryptocrystalline basalt, structural fissure, X-shaped. |