基于母岩类型差异的深层砂砾岩储集体成岩演化机制——以渤海湾盆地车镇凹陷沙河街组三段下亚段为例
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摘要
为探寻母岩类型对砂砾岩储集体成岩演化的控制作用,以渤海湾盆地车镇凹陷沙河街组三段下亚段为例,通过岩心全岩矿物X射线衍射、岩石薄片和流体包裹体等分析测试,系统分析了储集体的母岩类型、成岩环境及成岩演化机制。研究结果表明:车镇凹陷在沙河街组三段下亚段沉积期受控于母岩区埕子口凸起的差异构造升降和剥蚀作用,砂砾岩储集体的母岩由西向东依次发育碳酸盐岩、混合型和长英质3种类型;在不同母岩类型的砂砾岩储集体中,刚性颗粒和可溶矿物含量的不同决定了储集体自身的抗压实能力及其可溶于酸性流体的差异;在碱性—酸性—碱性成岩环境的交替影响下,刚性颗粒的支撑可有效沟通酸性流体,酸性流体与可溶矿物的水岩作用可形成次生孔隙;受控于刚性颗粒与可溶矿物的发育条件,各类型储集体的成岩演化机制存在差异;碳酸盐岩母岩型储集体、长英质母岩型储集体和母岩混合型储集体的有利储层在纵向上分别位于3 200 m、3 800 m和4 400 m以浅区域,平面上,母岩混合型储集体、长英质母岩型储集体、碳酸盐岩母岩型储集体的有利储层范围依次递减,各类型储集体的勘探方向存在差异。
Taking the lower submember of Member 3 of Shahejie Formation in Chezhen sag of Bohai Bay Basin as an example,and based on the analysis and testing of core rock X-ray diffraction,thin sections and fluid inclusions,this paper systematically analyzes the parent rock type,diagenetic environment and diagenetic evolution mechanism of the reservoir,so as to explore the control effect of parent rock type on diagenetic evolution of glutenite reservoir.The results show that the Chezhen sag is controlled by the differential tectonic uplift and denudation of Chengzikou uplift in the parent rock area during the sedimentary period of lower submember of Member 3 of Shahejie Formation.Three types of parent rock are successively developed in the glutenite reservoir,shown as carbonate rock-based,hybrid rock-based and felsic rock-based reservoirs from the west to the east;in the glutenite reservoirs of different parent rock types,the difference in the content of rigid particles and soluble minerals determines the compressive capacity of reservoirs and their differences in the solubility in acidic fluids.Under the alternating influence of alkaline-acid-alkaline diagenetic environment,acidic fluids can be effectively communicated by the support of rigid particles,and secondary pores can be formed through the water-rock interaction between acidic fluids and soluble minerals.Controlled by the development conditions of rigid particles and soluble minerals,various types of reservoirs present different diagenetic evolution mechanisms.The favorable reservoirs in the carbonate rock-based reservoir,felsic rock-based reservoir and hybrid rock-based reservoir are vertically located in the shallow regions of3 200 m,3 800 m and 4 400 m;on the horizontal level,the scale of favorable reservoirs is successively decreased,and there are differences in the exploration direction among each type of reservoirs.
Taking the lower submember of Member 3 of Shahejie Formation in Chezhen sag of Bohai Bay Basin as an example,and based on the analysis and testing of core rock X-ray diffraction,thin sections and fluid inclusions,this paper systematically analyzes the parent rock type,diagenetic environment and diagenetic evolution mechanism of the reservoir,so as to explore the control effect of parent rock type on diagenetic evolution of glutenite reservoir.The results show that the Chezhen sag is controlled by the differential tectonic uplift and denudation of Chengzikou uplift in the parent rock area during the sedimentary period of lower submember of Member 3 of Shahejie Formation.Three types of parent rock are successively developed in the glutenite reservoir,shown as carbonate rock-based,hybrid rock-based and felsic rock-based reservoirs from the west to the east;in the glutenite reservoirs of different parent rock types,the difference in the content of rigid particles and soluble minerals determines the compressive capacity of reservoirs and their differences in the solubility in acidic fluids.Under the alternating influence of alkaline-acid-alkaline diagenetic environment,acidic fluids can be effectively communicated by the support of rigid particles,and secondary pores can be formed through the water-rock interaction between acidic fluids and soluble minerals.Controlled by the development conditions of rigid particles and soluble minerals,various types of reservoirs present different diagenetic evolution mechanisms.The favorable reservoirs in the carbonate rock-based reservoir,felsic rock-based reservoir and hybrid rock-based reservoir are vertically located in the shallow regions of3 200 m,3 800 m and 4 400 m;on the horizontal level,the scale of favorable reservoirs is successively decreased,and there are differences in the exploration direction among each type of reservoirs.
引文
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[7]王俊鹏，张荣虎，赵继龙，等．超深层致密砂岩储层裂缝定量评价及预测研究———以塔里木盆地克深气田为例[J]．天然气地球科学，2014,25(11):1735-1745.WANG Junpeng,ZHANG Ronghu,ZHAO Jilong,et al.Characteristics and evaluation of fractures in ultra-deep tight sandstone reservoir:taking Keshen gasfield in Tarim Basin,NW China as an example[J].Natural Gas Geoscience,2014,25(11):1735-1745.
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