Characteristics and controlling factors of low porosity and low permeability reservoir of the second member of Jialingjiang Formation in southern Sichuan Basin

  • WEN Huaguo ,
  • JIA Bin ,
  • JIANG Yiqin ,
  • JIN Jun ,
  • QI Liqi ,
  • LI Lulu
Expand
  • 1. State Key Laboratory of Petroleum Resource and Prospecting, China University of Petroleum, Beijing 102249, China; 2. College of Geosciences, China University of Petroleum, Beijing 102249, China; 3. Shunan Gas District, Southwest Oil and Gas Field Company, PetroChina, Luzhou 646000, Sichuan, China

Online published: 2014-08-15

Abstract

Based on core observation, casting thin sections, physical properties and logging data, this paper studied the petrologic characteristics, diagenesis, reservoir space types, physical properties and controlling factors of the reservoir of the second member of Jialingjiang Formation in southern Sichuan Basin. The results show that high-quality reservoir is mainly developed in dolomite, especially in oolitic dolomite and micritic dolomite. The formation of oolitic dolomite is related to early dolomitization, and that of micritic dolomite is due to the dolomitization of micrite along with burial. Reservoir spaces of oolitic dolomite include intragranular dissolved pore, and the main pore types of micritic dolomite are dissolved pores and intracrystalline dissolved pores. The reservoir has the properties of low porosity and low permeability. Reservoir qualities are affected by palaeohigh, sedimentary facies and diagenesis. The restricted platform dolomite in the southeastern palaeohigh and grain beaches are favorable reservoirs.

Cite this article

WEN Huaguo , JIA Bin , JIANG Yiqin , JIN Jun , QI Liqi , LI Lulu . Characteristics and controlling factors of low porosity and low permeability reservoir of the second member of Jialingjiang Formation in southern Sichuan Basin[J]. Lithologic Reservoirs, 2014 , 26(4) : 81 -87 . DOI: 10.3969/j.issn.1673-8926.2014.04.012

References

[1] 童崇光.四川盆地构造演化与油气聚集[M].北京:地质出版社,1992.
[2] 胡明毅,魏国齐,李思田,等.四川盆地嘉陵江组层序-岩相古地理特征和储层预测[J].沉积学报,2010,28(6):1145-1152.
[3] 鲍志东,冯增昭,李永铁.中国南方东部三叠纪古地理演化及其构造控制[J].石油大学学报:自然科学版,1999,23(4):19-21.
[4] 王文之,田景春,张翔,等.川南丹凤—塘河地区嘉陵江组沉积环境分析[J].岩性油气藏,2011,23(6):50-55.
[5] 魏国齐,刘德来,张林,等.四川盆地天然气分布规律与有利勘探领域[J].天然气地球科学,2005,16(4):437-442.
[6] 马永生,蔡勋育,赵培荣,等.四川盆地大中型天然气田分布特征与勘探方向[J].石油学报,2010,31(3):347-354.
[7] 徐国盛,何玉,袁海锋,等.四川盆地嘉陵江组天然气藏的形成与演化研究[J].西南石油大学学报:自然科学版,2011,33(2):171-178.
[8] 朱其,李国蓉,乔占峰,等.四川盆地泸州古隆起嘉陵江组储层特征研究[J].四川地质学报,2008,28(1):30-34.
[9] 陈宗清.论四川盆地下三叠统嘉陵江组三—四段天然气勘探[J].中国石油勘探,2008,3(6):1-11.
[10] 赵澄林,陈丽华,涂强,等.中国天然气储层[M].北京:石油工业出版社,1999.
[11] 魏国齐,杨威,张林,等.川东北飞仙关组鲕滩储层白云石化成因模式[J].天然气地球科学,2005,16(2):162-166.
[12] 高梅生,郑荣才,文华国,等.川东北下三叠统飞仙关组白云岩成因———来自岩石结构的证据[J].成都理工大学学报:自然科学版,2007,34(3):297-304.
[13] 祝海华,钟大康.四川盆地龙岗气田三叠系飞仙关组储集层特征及成因机理[J].古地理学报,2013,15(2):275-282.
[14] 林雄,侯中健,田景春.四川盆地下三叠统嘉陵江组储层成岩作用研究[J].西南石油大学学报:自然科学版,2009,31(2):8-12.
[15] 郑荣才,史建南,罗爱君,等.川东北地区白云岩储层地球化学特征对比研究[J].天然气工业,2008,28(11):16-21.
[16] 曾伟,黄先平,杨雨,等.川东北地区飞仙关组储集层中的埋藏溶蚀作用[J].天然气工业,2006,26(11):4-8.
[17] 张廷山,陈晓慧,姜照勇,等.泸州古隆起对贵州赤水地区早、中三叠世沉积环境和相带展布的控制[J].沉积学报,2008,26(4):583-592.
[18] 赵雪凤,朱光有,刘钦甫,等.深部海相碳酸盐岩储层孔隙发育的主控因素研究[J].天然气地球科学,2007,18(4):514-521.
[19] 黄思静,张雪花,刘丽红,等.碳酸盐成岩作用研究现状与前瞻[J].地学前缘,2009,16(5):219-231.
[20] 洪海涛,杨雨,刘鑫,等.四川盆地海相碳酸盐岩储层特征及控制因素[J].石油学报,2012,33(增刊2):64-73.
[21] 张学丰,刘波,蔡忠贤,等.白云岩化作用与碳酸盐岩储层物性[J].地质科技情报,2010,29(3):79-85.
[22] 马永生.四川盆地普光超大型气田的形成机制[J].石油学报,2007,28(2):9-14.
Outlines

/