Reservoir characteristics of the first member of Middle Permian Maokou Formation in Sichuan Basin and its periphery and inspirations to petroleum exploration, SW China |
SU Chengpeng,LI Rong,SHI Guoshan,JIA Huofu,SONG Xiaobo |
Fig. 4. Reservoir space types of marl layers in LMAs of the Mao 1 Member in Sichuan Basin. (a) Well JH1, 2906.77 m, dissolved pores of matrix, plane-polarized light; (b) Well YY9, 1779.64 m, intragranular dissolved pores of bioclast and dissolved pores of matrix, cross-polarized light; (c) Well JH1, 2895.58 m, intragranular dissolved pores of bioclast and dissolved pores of matrix, plane-polarized light; (d) Well YY9, 1782.30 m, intragranular dissolved pores of dolomites, plane-polarized light; (e) Well JH1, 2896.40 m, intragranular dissolved pores of dolomite and intergranular dissolved pores, plane-polarized light; (f) Well JH1, 2893.80 m, microfracture, casting thin section; (g) Well JH1, 2906.88 m, fractures of grain margin and diagenetic pores and fractures of clay mineral, scanning electron microscopy (SEM) by argon ion polishing; (h) Well JH1, 2907.78 m, dissolution pores and cracks in grain of calcite, SEM by argon ion polishing; (i) Well JH1, 2901.92 m, pores within organic matter, SEM by argon ion polishing. |