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碳酸盐成岩作用和成岩环境的研究不只是一个理论问题,而且具有重要的实际意义。多年来,许多研究者都试图应用这个理论去解决一些实际问题。例如,成岩作用与油气的关系(Lowry,1956;Scholten,1959;Wilson,1977);成岩作用与沉积矿产关系(Taupitz,1954等);成岩作用与古地理和地层的对比(Dunham,J.B.1978等)。下面对这些问题作一些简要介绍。一、碳酸盐成岩环境与油气自沉积作用之后,在成岩作用过程中,分散的油气要运移到一定的部位,构成工业油气。这个过程正好发生在成岩作用过程中。显然,成岩作用的过程对油的聚集和分布有着明显的影响。
Carbonate diagenesis and diagenetic environment is not only a theoretical issue, but also has important practical significance. Over the years, many researchers have tried to apply this theory to solve some practical problems. For example, the relationship between diagenesis and hydrocarbon (Lowry, 1956; Scholten, 1959; Wilson, 1977); the relationship between diagenesis and sedimentary minerals (Taupitz, 1954, etc.); diagenesis versus palaeogeography and stratigraphy ). Here’s a brief introduction to these questions. First, the carbonate diagenetic environment and the role of hydrocarbon self-sedimentation, diagenesis in the process, the dispersed oil and gas to be transported to a certain site, constitute industrial oil and gas. This process occurs exactly in the process of diagenesis. Obviously, the process of diagenesis has a significant impact on the oil accumulation and distribution.