川东地区五百梯构造带长兴组有利储集相带预测
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摘要
川东地区五百梯构造带上二叠统长兴组为川东地区天然气藏的主要产层,也是邻区寻找新气源的最有利层位之一。根据野外剖面、岩心和室内镜下岩石薄片鉴定分析,并结合岩石学、测井及地震等沉积相标志研究,确定五百梯构造带长兴组发育有台内海槽(深水盆地)、台地前缘缓斜坡、台地边缘生物礁滩和开阔台地4个沉积相带,进一步划分出若干亚相和微相。研究认为,岩石类型、沉积环境和成岩作用对储集层具有明显的影响,长兴组台地边缘生物礁滩相地层为最重要的油气勘探层段,骨架礁、黏结礁和生屑滩为最有利储层发育的微相,储层岩性主要为颗粒白云岩、晶粒白云岩和礁白云岩。在此基础上,综合考虑各种因素,以结合地质资料预测的沉积相平面分布图叠合地震反演预测的生物礁滩岩隆带,最终圈定出有利储集相带发育区。
The characteristics and genesis of the reservoirs in Changxing Formation in the Wubaiti area are studied.The Changxing Formation of Permain is the major pay zone of the gas fields in the eastern Sichuan Basin and also one of the most favorable targets for gas exploration in the adjacent areas.Based on outcrop observation,core description and thin section analysis in combination with lithological,palaeontological and logging data,the Changxing Formation is divided into four main sedimentary facies,i.e.the facies of intratrough platform(deep water basin),platform slope,platform edge and open platform.Various subfacies and microfacies could be further recognized.The reservoir properties of the Changxing Formation are generally controlled by microfacies and diagenesis.Reef flat deposits,reef framework and bindstones are favorable microfacies for reservoir space.The rock types of reservoir mainly consist of grained dolomite,reef dolomite and sparry dolomite.It is conclued that favorite reservoirs could be predicted by the integrated study of all factors,in particular the spatial distribution pattern of depositional facies,the detailed facies framework of the bioreef deposits and the thickness distribution of dolomite inferred from seismic data.
The characteristics and genesis of the reservoirs in Changxing Formation in the Wubaiti area are studied.The Changxing Formation of Permain is the major pay zone of the gas fields in the eastern Sichuan Basin and also one of the most favorable targets for gas exploration in the adjacent areas.Based on outcrop observation,core description and thin section analysis in combination with lithological,palaeontological and logging data,the Changxing Formation is divided into four main sedimentary facies,i.e.the facies of intratrough platform(deep water basin),platform slope,platform edge and open platform.Various subfacies and microfacies could be further recognized.The reservoir properties of the Changxing Formation are generally controlled by microfacies and diagenesis.Reef flat deposits,reef framework and bindstones are favorable microfacies for reservoir space.The rock types of reservoir mainly consist of grained dolomite,reef dolomite and sparry dolomite.It is conclued that favorite reservoirs could be predicted by the integrated study of all factors,in particular the spatial distribution pattern of depositional facies,the detailed facies framework of the bioreef deposits and the thickness distribution of dolomite inferred from seismic data.
引文
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[2]王一刚,文应初,张帆.川东地区上二叠统长兴组生物礁分布规律[J],天然气工业,1998,18(6):10-15.
[3]王一刚,张静,杨雨,等.四川盆地东部上二叠统长兴组生物礁气藏形成机理[J].海相油气地质,1997,5(1):145-152.
[4]倪新风,陈洪德,田景春,等.川东北地区飞仙关组—长兴组沉积格局与成藏控制意义[J],石油与天然气地质,2007,28(4):458-167.
[5]牟传龙,谭钦银,余谦,等.川东北地区上二叠统长兴组生物礁组成及成礁模式[J].沉积与特提斯地质,2004,24(3):65-71.
[6]周刚,郑荣才,王炯,等.川东—渝北地区长兴组礁、滩相储层预测[J].岩性油气藏,2009,21(1):15-21.
[7]张兵,郑荣才,文华国,等.开江—梁平台内海槽东段长兴组礁滩相储层识别标志及其预测[J].高校地质学报,2009,15(2):273-284.
[8]任兴国,罗利,姚声贤,等.川东地区生物礁测井预测方法研究[J],石油勘探与开发,2000,27(01):41-43.
[9]蒋晓光,彭大钧,陈季高,等.滨里海盆地东缘生物礁预测研究[J].成都理工大学学报,2005,32(5):492-497.
[10]陈劲人,银玉光.建南气田长兴组生物礁气藏的勘探实践[J].石油勘探与开发,1981,10(2):27-33.
[11]刘划一,王一刚,杨雨,等.川东上二叠统生物礁气藏多元信息综合预测方法研究[J].天然气工业,1999,19(4):13-18.
[12]Aminzhadeh F.将气囱作为一种勘探工具[J].陆光辉,译.石油勘探开发情报,2001(6):22-32.
[13]姜在兴.沉积学[M].北京:石油工业出版社,2003,404-420.
[14]马永生,牟传龙,郭旭升,等.川东北地区长兴组沉积特征与沉积格局[J].地质论评,2006,52(1):25-29.
[15]王瑞华,牟传龙,谭钦银,等.达县—宣汉地区长兴组礁滩白云岩成岩作用与成岩环境研究[J].沉积与特提斯地质,2006,26(1):30-36.
[16]郑荣才,胡忠贵,冯青平,等.川东北地区长兴组白云岩储层的成因研究[J].矿物岩石,2007,27(4):78-84.
[17]雷卞军,强子同,文应初.川东及邻区上二叠统生物礁的白云岩化[J].地质论评,1999,40(6):534-543.
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