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塔里木和四川盆地白云岩规模优质储层形成与发育控制因素
引用本文:乔占峰,张哨楠,沈安江,佘敏,黄理力,李文正,邵冠铭,戴传瑞. 塔里木和四川盆地白云岩规模优质储层形成与发育控制因素[J]. 石油与天然气地质, 2022, 43(1): 92-104. DOI: 10.11743/ogg20220108
作者姓名:乔占峰  张哨楠  沈安江  佘敏  黄理力  李文正  邵冠铭  戴传瑞
作者单位:1.西南石油大学 油气藏地质及开发工程国家重点实验室, 四川 成都 6105002.中国石油 杭州地质研究院, 浙江 杭州 3100233.中国石油天然气集团公司 碳酸盐岩储层重点实验室, 浙江 杭州 310023
基金项目:国家科技重大专项(2016ZX05004-002);中国石油重点科技项目(2019B-0406);中国石油基础性前瞻性科技项目(2021DJ0503)。
摘    要:通过对塔里木和四川盆地典型实例的对比,基于白云石化作用与孔隙形成机制和期次的分析,梳理了白云岩规模优质储层发育控制因素,提出了准同生期白云石化作用是储层规模化发育的关键;溶蚀作用是提升白云岩储层质量的必要条件;规模优质储层发育的前提在于白云石化作用和溶蚀作用发生的耦合关系.提出3种有利于规模优质白云岩储层发育的地质过程...

关 键 词:白云岩储层  白云石化  埋藏云化  深层白云岩  四川盆地  塔里木盆地
收稿时间:2020-03-30

Controls on formation and development of large-sized high-quality dolomite reservoirs in the Tarim and Sichuan Basins
Qiao Zhanfeng,Zhang Shaonan,Shen Anjiang,She Min,Huang Lili,Li Wenzheng,Shao Guanming,Dai Chuanrui. Controls on formation and development of large-sized high-quality dolomite reservoirs in the Tarim and Sichuan Basins[J]. Oil & Gas Geology, 2022, 43(1): 92-104. DOI: 10.11743/ogg20220108
Authors:Qiao Zhanfeng  Zhang Shaonan  Shen Anjiang  She Min  Huang Lili  Li Wenzheng  Shao Guanming  Dai Chuanrui
Affiliation:1.State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Southwest Petroleum University, Chengdu, Sichuan 610500, China2.Hangzhou Research Institute of Geology, PetroChina, Hangzhou, Zhejiang 310023, China3.Key Laboratory of Carbonate Reservoirs, CNPC, Hangzhou, Zhejiang 310023, China
Abstract:Following a comparative analysis of the main mechanisms and periods of dolomitization and dissolution in typical dolomite reservoirs in Tarim and Sichuan Basins,we identified the factors controlling the development of large-sized high-quality dolomite reservoirs: penecontemporaneous dolomitization is crucial to the scale of the reservoirs and dissolution modification is necessary for the quality of the reservoirs,thus the coupling of dolomitization with dissolution is the prerequisite for the development of large and high-quality dolomite reservoirs.Three geological processes that facilitate the development of the reservoirs were also brought forward: the (pene-) contemporaneous dolomitization associated with dissolution that mainly formed high-energy mound/reef-shoal and tidal-flat reservoirs against the backdrop of sea level fall; the adoptive burial dolomitization that mostly created reservoirs through shallow dolomitization of preexisting reservoirs,with quality and scale conditioned by the facies and dissolution intensity of preexisting reservoirs; and the epigenetic modification by dissolution that formed reservoirs after a hydrothermal or meteoric karstification of preexisting dolomite reservoirs,with quality and size controlled by facies,faults and unconformities as well as the development of the preexisting dolomite reservoirs.The above understandings may shed light on the prediction of large-sized deep high-quality dolomite reservoirs.
Keywords:dolomite reservoir  dolomitization  burial dolomitization  deep dolomite  Tarim Basin  Sichuan Basin
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