因而认为地表、近地表方解石充填过程是碳酸盐岩洞穴型储层的“保持性成岩作用”。

So, the calcite filling in surface and near-surface is "retention diagenesis" of carbonate cavern reservoir.

youdao

因而认为地表、近地表方解石充填过程是碳酸盐岩洞穴型储层的“保持性成岩作用”。

So, the calcite filling in surface and near-surface is "retention diagenesis" of carbonate cavern reservoir.

youdao