不同体系域碎屑岩储集体成岩演化差异——以渤南洼陷沙三段为例
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摘要
为探究原始沉积组分与水体环境对碎屑岩储集体成岩演化的影响,以济阳坳陷渤南洼陷沙三段为例,综合运用钻井、测井以及大量分析化验资料开展了相关研究。结果表明:渤南洼陷沙三段湖侵域沉积期为近源、半咸水沉积环境,碎屑岩储集体富含碳酸盐岩屑,抗压实能力较弱,加之半咸水环境,使其在成岩早期经历了较强压实与胶结成岩作用,原生孔隙递减快,在成岩中期无足够空间容纳有机酸,酸性溶蚀作用较弱,现今储集体物性差;高位域沉积期为远源、淡水沉积环境,碎屑岩储集体以石英颗粒为主,抗压实能力较强,加之淡水环境,使其在成岩早期经历了弱压实与胶结成岩作用,原生孔隙递减慢,成岩中期酸性溶蚀作用较强,现今储集体物性较好。原始沉积组分与水体环境是导致碎屑岩储集体成岩演化差异的本质因素。
In order to clarify the influence of original sedimentary components and water environment on diagenetic evolu-tion of clastic reservoirs,the 3 rd member of Shahejie Formation of Paleogene in Bonan Sag,Jiyang Depression was analyzedwith drilling,logging and a large number of testing data in detail. The results show that the lowstand systems tract of the 3 rdmember of Shahejie Formation in Bonan Sag is in a near-subaqueous and brackish water sedimentary environment. Theclastic reservoir is rich in carbonate rock debris and has low resistance to compaction. In addition,the brackish water envi-ronment makes it undergo strong compaction and cementation diagenesis in the early diagenetic stage. The primary porosityof reservoir decreases rapidly and there is not enough space to accommodate organic acids in the middle diagenetic stage.The acid dissolution is weak and the reservoir physical properties are poor at present. The highstand systems tract of the 3 rdmember of Shahejie Formation in Bonan Sag is a long-distance and freshwater sedimentary environment. Clastic reservoiris dominated by quartz particles and has high resistance to compaction. In addition,the freshwater environment makes it un-dergo weak compaction and cementation diagenesis in the early diagenetic stage. So the primary porosity of reservoir de-clines slowly. The reservoir experiences strong acid corrosion in the middle stage of diagenesis and the reservoir physicalproperties are good at present. The original sedimentary components and water environment are the essential factors leadingto the differences in diagenetic evolution of the clastic reservoirs.
In order to clarify the influence of original sedimentary components and water environment on diagenetic evolu-tion of clastic reservoirs,the 3 rd member of Shahejie Formation of Paleogene in Bonan Sag,Jiyang Depression was analyzedwith drilling,logging and a large number of testing data in detail. The results show that the lowstand systems tract of the 3 rdmember of Shahejie Formation in Bonan Sag is in a near-subaqueous and brackish water sedimentary environment. Theclastic reservoir is rich in carbonate rock debris and has low resistance to compaction. In addition,the brackish water envi-ronment makes it undergo strong compaction and cementation diagenesis in the early diagenetic stage. The primary porosityof reservoir decreases rapidly and there is not enough space to accommodate organic acids in the middle diagenetic stage.The acid dissolution is weak and the reservoir physical properties are poor at present. The highstand systems tract of the 3 rdmember of Shahejie Formation in Bonan Sag is a long-distance and freshwater sedimentary environment. Clastic reservoiris dominated by quartz particles and has high resistance to compaction. In addition,the freshwater environment makes it un-dergo weak compaction and cementation diagenesis in the early diagenetic stage. So the primary porosity of reservoir de-clines slowly. The reservoir experiences strong acid corrosion in the middle stage of diagenesis and the reservoir physicalproperties are good at present. The original sedimentary components and water environment are the essential factors leadingto the differences in diagenetic evolution of the clastic reservoirs.
引文
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