Carbonate reservoirs can be divided into intra-sequence reservoirs and sequence boundary reservoirs based on study of sequence stratigraphy.
利用层序地层学研究可将碳酸盐岩储层分为层序内部储层和层序界面储层。
Carbonate reservoirs can be divided into intra-sequence reservoirs and sequence boundary reservoirs based on study of sequence stratigraphy.
利用层序地层学研究可将碳酸盐岩储层分为层序内部储层和层序界面储层。
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