Reservoir diagenesis of 3rd member of Feixianguan Formation, Jiannan Gas Field
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摘要: 以建43井为例,研究了建南气田三叠系飞三段储层的成岩作用及特点,其中白云岩化作用、溶蚀作用和构造破裂作用对储层贡献较大。其成岩序列为藻粘结、泥晶化→一世代胶结→大气淡水溶蚀→二世代粒状胶结→新生变形→压实压溶→白云岩化→早期张裂缝及充填→构造挤压作用→埋藏溶蚀Ⅰ→进油→白云石、萤石充填、石英充填交代→油演化为沥青→埋藏溶蚀Ⅱ→晚期张裂缝→进气;主要经历了海底(潮间)环境、大气淡水环境、浅埋藏和深埋藏环境。白云石晶体、二世代粒状胶结物、萤石被溶蚀、压性裂缝发育以及孔隙无明显变形是埋藏溶蚀的主要识别标志。Abstract: Diagenesis and features of the 3rd member of Feixianguan Formation in the Jiannan Gas Field were studied taking well Jian43 as an example.Dolomitization,karstification and tectonic disruption were contributive to reservoir.Diagenesis sequence was illustrated as follows: algae agglutinate and micritization→first consolidation→atmospheric water erosion→secondary granular consolidation→neomorphism→compaction and pressolution→dolomitization→early tension fissure and filling→tectonic compression→buried erosion Ⅰ→petroleum entering→dolomite and fluorite filling as well as quartz filling and metasomatism→oil evolving to bitumen→buried erosion Ⅱ→late tension fissure→gas entering.There were 4 kinds of diagenesis environment including seabed (intertidal),atmospheric water,shallow bury and deep bury.Dolomite crystals,secondary granular consolidations,eroded fluorites,tensional fissures and pores without obvious deformation were the main identifications for buried erosions.
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[1] 丁道桂,郭彤楼,翟常博,等.鄂西—渝东区膝折构造[J].石油实验地质,2005,27(3):205-210. [2] 盛贤才,王韶华,文可东,等.鄂西渝东地区石柱古隆起构造沉积演化[J].海相油气地质,2004(1-2):43-52. [3] 胡纯心,高林,刘锐.鄂西渝东区构造特征及其发展演化[J].江汉石油科技,2000,10(2):59-62. [4] 王韶华,万云强,林娟华.建南气田海相天然气藏成因类型探讨[J].石油天然气学报,2008,30(4):37-42. [5] 陈学辉,张毅.鄂西建南地区天然气勘探成果认识与勘探目标[J].江汉石油职工大学学报,2006,19(4):10-12. [6] 梁西文,郑荣才.建南构造飞仙关组三段高精度层序地层学及南北高点储层差异原因探讨[J].沉积与特提斯地质,2006,26(3):45-50. [7] 曾庆立.建南气田周缘地区飞仙关组沉积特征与勘探目标[J].江汉石油职工大学学报,2004,17(2):8-9. [8] 倪新锋,陈洪德,田景春,等.川东北地区长兴组—飞仙关组沉积格局及成藏控制意义[J].石油与天然气地质,2007,28(4):458-465. [9] 万云强,殷文洁,陈明剑.建南地区低孔低渗储集层改造技术应用效果分析[J].石油天然气学报,2005,27(2):249-250. [10] 范松之,韦林波.建南地区飞三段储层的测井评价[J].江汉石油科技,2002,12(3):25-28.
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