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Major factors controlling the formation of middle and large marine carbonate stratigraphic fields

机译:控制中大型海相碳酸盐岩地层形成的主要因素

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摘要

Marine carbonate oil and gas fields have become an important exploration area in China and even across the world. Their formation, distribution and enrichment are special owing to the complexity of the deposition, diagenesis and accumulation, which iscaused by the multiplicity of the carbonate de-positional environments and facies, huge extensions of formation time and burial depth, complication of diagenetic evolution, heterogeneity as well as the development of pores, caves and fractures affectedby various factors. Oil and gas accumulations in carbonate rocks are not strictly controlled by the second-order structure belt. Most of them, under certain structural settings, are controlled by sedimentary diagenesis and its favorable facies. The hydrocarbon reservoir type is predominantly stratigraphic. Based on the worldwide researches of carbonate fields, the paper concludes that 7 main factors control the formation and distribution of middle-large marine carbonate stratigraphic fields.
机译:海洋碳酸盐岩油气田已经成为中国乃至全球的重要勘探领域。由于沉积,成岩作用和堆积的复杂性,它们的形成,分布和富集是特殊的,这是由于碳酸盐沉积环境和相的多样性,形成时间和埋藏深度的大量延长,成岩演化的复杂性,异质性造成的。以及受各种因素影响的孔隙,洞穴和裂缝的发育。碳酸盐岩中的油气聚集不受二阶构造带的严格控制。在一定的构造背景下,它们中的大多数受沉积成岩作用及其有利相的控制。碳氢化合物储层类型主要为地层。基于对全球碳酸盐岩田的研究,得出以下7个主要因素控制中大型海相碳酸盐岩地层的形成和分布。

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