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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
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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