松辽盆地南部东南隆起区储层特征

杨铭辉; 郭力; 赵洪涛; 史雅丽; 张坤

doi:10.11781/sysydz200604330

松辽盆地南部东南隆起区储层特征

doi: 10.11781/sysydz200604330

1.
中国地质大学地球科学与资源学院, 北京 100083
2. 中国石油天然气股份有限公司吉林油田分公司新民采油厂, 吉林松原 138000
3. 中国石油天然气股份有限公司吉林油田分公司科技与信息处, 吉林松原 138000
4. 中国石油天然气集团公司吉林石油集团有限责任公司试油测试公司, 吉林松原 138000
5. 中国石油天然气股份有限公司吉林油田分公司勘探开发研究院, 吉林松原 138000

详细信息

作者简介:
杨铭辉(1966- ),男(汉族),吉林松原人,博士生,主要从事油气地质综合研究.

中图分类号: TE122.2
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出版历程
- 收稿日期: 2005-08-04
- 修回日期: 2006-07-03
- 刊出日期: 2006-07-28

RESERVOIR CHARACTERISTICS IN THE SE UPLIFT, THE SOUTH OF SONGLIAO BASIN

1.
School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China
2. Xinmin Oil Recovery Factory, Jilin Oil Field Branch Company, PetroChina Songyuan, Jilin 138000, China
3. Technology and Information Bureau, Jilin Oil Field Branch Company, PetroChina Songyuan, Jilin 138000, China
4. Oil Testing Company, Jilin Petroleum Cooperation Ltd, CNPC, Songyuan, Jilin 138000, China
5. Research Institute of Petroleum Exploration and Development, Jilin Oil Field Branch Company, PetroChina, Songyuan, Jilin 138000, China

摘要

摘要: 松辽盆地南部东南隆起区深层发育4种类型的储层,以往的勘探成果证实,砂岩、砂砾岩是主要储集层.各断陷的岩石类型主要为岩屑长石砂岩和长石岩屑砂岩.成岩作用强烈,不同程度地改变了储层的储集性能.由于各种因素的影响,盆地东南深层的砂岩和砂砾岩储层中,发育3个次生孔隙发育带,不同程度地改善了储层的储集条件.综合评价认为,各断陷中泉头组一段储层的物性相对较好,应是今后勘探的主要目的层;王府断陷各层位的储层物性相对较差.
- 砂砾岩 /
- 火山岩 /
- 变质岩 /
- 储层 /
- 次生孔隙 /
- 成岩作用 /
- 松辽盆地
Abstract: Four types of reservoir have been generated deep in the SE uplift,the south of Songliao Basin.The previous studies have indicated that,sandstone and glutinite are the major reservoirs.The rocks in different faults are mainly detritus feldspar sandstone and feldspar detritus sandstone.Strong diagenesis changes reservoir ability to different extents.Due to the influence of various factors,three induced porosity zones,which have improved the storing ability of reservoir to different extents,have been developed in the reservoirs of sandstone and glutinite located in the southeast deep layer.It can be concluded through comprehensive evaluation that,the physical performance of reservoir bed in the first part of Quantou Formation in various faults is relatively better and it should be the major objective layer in future exploration.Physical performance of all layers in the Wangfu fault is relatively worse.
- reservoir /
- glutinite /
- induced porosity /
- diagenesis /
- volcanic rock /
- metamorphics /
- the Songliao Basin

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参考文献(7)

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