Dissolution of feldspar and lithic fragment make the pores linking. Diagenesis has reached the late diagenesis the stage A.

巴什基奇克组为偏碱性成岩环境，压实和胶结作用中等偏弱，溶蚀作用改善了孔隙结构，成岩阶段达晚成岩A期。

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Dissolution of feldspar and lithic fragment make the pores linking. Diagenesis has reached the late diagenesis the stage A.

巴什基奇克组为偏碱性成岩环境，压实和胶结作用中等偏弱，溶蚀作用改善了孔隙结构，成岩阶段达晚成岩A期。

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