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。
Besides the macroscopic sedimentary records analytical methods, the sequence boundary and inter systems tract can also be identified by microcosmic analysis information of sedimentary geochemistry.
层序界面和层序内体系域的识别除宏观的沉积记录分析方法外，还可通过微观的沉积地球化学分析资料来识别。
The characters of the two sequence stratigraphy on theoretical basis, sequence order and sequence boundary also shows that there has great possibility theoretically on their syncretization.
对两种层序地层学理论基础、层序级次、层序界面等特征分析表明，这两种层序地层学理论上具有相互结合的可能性。
The characters of the two sequence stratigraphy on theoretical basis, sequence order and sequence boundary also shows that there has great possibility theoretically on their syncretization.
对两种层序地层学理论基础、层序级次、层序界面等特征分析表明，这两种层序地层学理论上具有相互结合的可能性。
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