Dolomitization evolution and its effects on hydrocarbon reservoir formation from penecontemporaneous to deep burial environment

作     者：SHEN Anjiang LUO Xianying HU Anping QIAO Zhanfeng ZHANG Jie SHEN Anjiang;LUO Xianying;HU Anping;QIAO Zhanfeng;ZHANG Jie

作者机构：PetroChina Hangzhou Institute of Petroleum GeologyHangzhou 310023China Key Laboratory of Carbonate ReservoirsCNPCHangzhou 310023China 

出 版 物：《Petroleum Exploration and Development》 (石油勘探与开发（英文版）)

年 卷 期：2022年第49卷第4期

页      面：731-743页

核心收录：

学科分类：0820[工学-石油与天然气工程] 081803[工学-地质工程] 08[工学] 0818[工学-地质资源与地质工程] 0708[理学-地球物理学] 

基　　金：Supported by the China National Science and Technology Major Project(2016ZX05004-002) PetroChina Science and Technology Project(2019-5009-16). 

主　　题：dolomitization dolomitization pathway dolomite reservoir carbonates penecontemporaneous environment burial environment dolomite genesis identification template 

摘      要：Aiming at the scientific problem that only part of dolomite acts as dolomite reservoir,this paper takes the multiple dolomite-bearing formations in the Tarim and Ordos basins,NW China and Sichuan Basin,SW China as the study object,by means of mineral petrological analysis and geochemical methods including carbonate clumped isotope,U-Pb isotopic dating,etc.,to rebuild the dolomitization pathway and evaluate its effects on reservoir formation.On the basis of detailed rock thin section observation,five dolomitic structural components are identified,including original fabric-retained dolomite(microbial and/or micrite structure),buried metasomatic dolomite I(subhedral-euhedral fine,medium and coarse crystalline structure),buried metasomatic dolomite II(allotriomorphic-subhedral fine,medium and coarse crystalline structure),buried precipitation dolomite and coarse crystalline saddle dolomite.Among them,the first three exist in the form of rocks,the latter two occur as dolomite minerals filling in pores and fractures.The corresponding petrological and geochemical identification templates for them are established.Based on the identification of the five dolomitic structural components,six dolomitization pathways for three types of reservoirs(preserved dolomite,reworked dolomite and limestone buried dolomitization)are distinguished.The initial porosity of the original rock before dolomitization and the dolomitization pathway are the main factors controlling the development of dolomite reservoirs.The preserved dolomite and reworked dolomite types have the most favorable dolomitization pathway for reservoir formation,and are large scale and controlled by sedimentary facies in development and distribution,making them the first choices for oil and gas exploration in deep carbonate formations.