西南石油大学学报(自然科学版)
西南石油大學學報(自然科學版)
서남석유대학학보(자연과학판)
JOURNAL OF SOUTHWEST PETROLEUM UNIVERSITY(SEIENCE & TECHNOLOGY EDITION)
2014年
1期
27-32
,共6页
黄东%李红亮%蒋静萍%石学文%汪华
黃東%李紅亮%蔣靜萍%石學文%汪華
황동%리홍량%장정평%석학문%왕화
地层厘定%储集性能%滩相%运移聚集%雷一 1%川西北
地層釐定%儲集性能%灘相%運移聚集%雷一 1%川西北
지층전정%저집성능%탄상%운이취집%뢰일 1%천서북
formation determination%reservoir performance%shoal facies%migration and accumulation%T2l11%northwestern Sichuan
四川盆地雷口坡组资源量大,除勘探早期发现卧龙河、磨溪雷一1气藏外,其余地方尚未在雷一段获得规模储量。随着川西地区海相层系勘探步伐的加快,特别是川西北地区勘探程度的深入,雷一1逐渐显示出良好的勘探前景。在川西北雷口坡组地层厘定的基础上,根据野外剖面、岩屑样品、钻井和试油等资料,认为川西北地区雷一1储层有着与川中磨溪、川东卧龙河相似或者相当的储集性能,均属于受滩相控制的储层。与此同时,该区经历了多期次的构造运动,构造圈闭、断层发育,有利于油气的运移和聚集,综合分析后认为,龙门山前缘中北段的中坝-双鱼石以及米仓山前缘的梅树铺-九龙山一带是最有利的勘探区带。
四川盆地雷口坡組資源量大,除勘探早期髮現臥龍河、磨溪雷一1氣藏外,其餘地方尚未在雷一段穫得規模儲量。隨著川西地區海相層繫勘探步伐的加快,特彆是川西北地區勘探程度的深入,雷一1逐漸顯示齣良好的勘探前景。在川西北雷口坡組地層釐定的基礎上,根據野外剖麵、巖屑樣品、鑽井和試油等資料,認為川西北地區雷一1儲層有著與川中磨溪、川東臥龍河相似或者相噹的儲集性能,均屬于受灘相控製的儲層。與此同時,該區經歷瞭多期次的構造運動,構造圈閉、斷層髮育,有利于油氣的運移和聚集,綜閤分析後認為,龍門山前緣中北段的中壩-雙魚石以及米倉山前緣的梅樹鋪-九龍山一帶是最有利的勘探區帶。
사천분지뢰구파조자원량대,제감탐조기발현와룡하、마계뢰일1기장외,기여지방상미재뢰일단획득규모저량。수착천서지구해상층계감탐보벌적가쾌,특별시천서북지구감탐정도적심입,뢰일1축점현시출량호적감탐전경。재천서북뢰구파조지층전정적기출상,근거야외부면、암설양품、찬정화시유등자료,인위천서북지구뢰일1저층유착여천중마계、천동와룡하상사혹자상당적저집성능,균속우수탄상공제적저층。여차동시,해구경력료다기차적구조운동,구조권폐、단층발육,유리우유기적운이화취집,종합분석후인위,룡문산전연중북단적중패-쌍어석이급미창산전연적매수포-구룡산일대시최유리적감탐구대。
Leikoupo Formation has a large amount of resources,but in addition to the previously found Wolonghe,Moxi gas reservoir,no other reserve of scale has been found. With the progress of exploration of the marine strata in western Sichuan,es-pecially further degree of exploration,the T2l11 gradually exhibits its good exploration prospects. Based on Leikoupo Formation determination,and according the field profile,debris samples,oil drilling and test data analysis,we think that the sub-section of the T2l11 belongs to the reservoir controlled by shale facies which is similar or equivalent to Moxi and Wolonghe reservoirs. Structural traps and fault development in the area are conducive to oil and gas migration and accumulation. Comprehensive analysis reveals that the most favorable exploration zones are the Zhongba-Shuangyushi belt in the front north of Longmen mountain and the Meishupu-Jiulongshan belt in the front of Micangshan mountain.