Carbonate reservoirs can be divided into intra-sequence reservoirs and sequenceboundary 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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The characters of the two sequence stratigraphy on theoretical basis, sequence order and sequenceboundary also shows that there has great possibility theoretically on their syncretization.
Besides the macroscopic sedimentary records analytical methods, the sequenceboundary and inter systems tract can also be identified by microcosmic analysis information of sedimentary geochemistry.