而溶蚀作用从一定程度上使储层物性得到了改善，次生孔隙相对增多。
To some extent, the chemical erosion made the physical property of reservoir getting better and increased the secondary pore relatively.
成岩环境在一定程度上影响了水岩反应及次生孔隙发育。
The diagenetic environment results in different water-rock reaction and development of secondary porosity.
火山岩原生和次生孔隙使其可成为储集层，在一定条件下可成为盖层。
The primary and secondary pores of volcanic rocks provided reservoir space there. Volcanic rock may become cap rock under certain conditions.
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