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Genetic types and distinguished characteristics of dolomite and the origin of dolomite reservoirs

机译:白云岩成因类型,特征及白云岩储层成因

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To find out the origin of dolomite, the precipitation of primary dolomite, and the formation of pores in dolomite, petrologic and geochemical characteristics of typical samples from Sichuan and Tarim Basin were analyzed based on the previous understandings, and three aspects of results were achieved. (1) A classification of dolomite origins based on petrologic features, forming environment, and time sequence was proposed, which shows clear boundaries of diagenetic and characteristic realms and evolved clues between different types of dolomite. (2) Petrographic and geochemical identification marks for different types of dolomite were presented, revealing that the orderly geochemical variation of different types of dolomite is the response to the change of forming environment of dolomite during continuous time sequence. (3) The contribution of dolomitization to the formation of porosity was re-evaluated, revealing that the porosity in dolomite was mostly attributed to the primary pores and supergene dissolution and burial dissolution, and early dolomitization was conducive to the preservation of primary pores. These understandings are of great theoretical significance for identifying the origins and types of dolomite, and can guide the prediction of dolomite reservoirs.
机译:为了了解白云岩的成因,原生白云岩的沉淀以及白云岩中孔隙的形成,在对四川和塔里木盆地典型样品的岩性和地球化学特征的基础上,根据先前的认识,进行了分析,得出了三个方面的结果。 (1)提出了根据岩石学特征,形成环境和时间顺序对白云岩成因进行分类的方法,该分类法清楚地显示了成岩和特征领域的清晰边界,以及不同类型白云岩之间的演化线索。 (2)给出了不同类型白云岩的岩石学和地球化学识别标记,揭示了不同类型白云岩的有序地球化学变化是对连续时间序列中白云石形成环境变化的响应。 (3)重新评估了白云石化对孔隙形成的贡献,发现白云岩的孔隙度主要归因于原生孔隙和表生溶蚀作用和埋藏溶解作用,早期白云石化有利于原生孔隙的保存。这些认识对识别白云岩的成因和类型具有重要的理论意义,可以指导白云岩储层的预测。

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