Sandstone has entered the late diagenesis Asubage period.
砂岩已进入晚成岩a亚期阶段。
The rocks have experienced early diagenesis, epidiagenesis and late diagenesis.
岩石经历了早期成岩作用、表生成岩作用和晚期成岩作用。
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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