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石油实验地质  2014, Vol. 36 Issue (1): 25-32    DOI: 10.11781/sysydz201401025
盆地·油藏 本期目录 | 过刊浏览 |
准噶尔盆地隐蔽油气藏类型及有利勘探区带
刘传虎
中国石油化工股份有限公司 胜利油田分公司, 山东 东营 257001
Subtle reservoir type and favorable exploration belts in Junggar Basin
Liu Chuanhu
SINOPEC Shengli Oilfield Company, Dongying, Shandong 257001, China
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摘要: 针对准噶尔盆地隐蔽油气藏勘探潜力巨大但成藏规律非常复杂的情况,在回顾其隐蔽油气藏勘探历程基础上,把已发现的隐蔽油气藏划分为岩性类、地层类、复合类和(准)连续型4大类及17个亚类。其成藏特点为:多沉积体系控制;多圈闭类型展布、构造—岩性—地层复合;多层系含油气;多期充注、多期成藏;多成藏组合型式。隐蔽油气藏有利勘探区带为盆地西缘车排子斜坡带沙湾组成藏组合、车—莫古隆起周缘侏罗系成藏组合、准噶尔盆地石炭系成藏组合和北天山山前坳陷深层致密砂岩侏罗系成藏组合。
关键词 隐蔽油气藏类型成藏特点有利勘探区带准噶尔盆地    
Abstract:According to the great potential and complicated accumulation rules of subtle reservoirs in the Junggar Basin, we divided the discovered subtle reservoirs in the study area into 4 types (lithologic, stratigraphic, complex and quasi-continuous ones) and 17 subtypes based on previous exploration experiences. The accumulation characteristics were concluded as followed: the control of multiple sedimentary systems; the occurrence of multiple trap types and the combination of structural-lithologic-stratigraphic traps; multiple hydrocarbon bearing layers; multiple stages of hydrocarbon charging and accumulation; multiple oil and gas plays. The favorable exploration belts of subtle reservoirs include the Shawan Formation in the Chepaizi slope in the western margin of the basin, the Jurassic around the Che-Mo paleo-uplift, the Carboniferous in the Junggar Basin, and the Jurassic tight sandstones in the piedmont depression of the North Tianshan.
Key wordssubtle reservoir type    accumulation characteristics    favorable exploration belt    Junggar Basin
收稿日期: 2013-03-15     
ZTFLH:  TE122.3  
基金资助:国家科技重大专项“准噶尔盆地碎屑岩层系大中型油气田形成规律与勘探方向”(2011ZX05002-002)和中国石化股份公司科研项目(P03011,P04033)联合资助。
作者简介: 刘传虎(1964-),男,博士,教授级高级工程师,从事油田勘探与管理工作。E-mail:liuchuanhu.slyt@sinopec.com。
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引用本文:

刘传虎. 准噶尔盆地隐蔽油气藏类型及有利勘探区带[J]. 石油实验地质, 2014, 36(1): 25-32.
Liu Chuanhu. Subtle reservoir type and favorable exploration belts in Junggar Basin. PETROLEUM GEOLOGY & EXPERIMENT, 2014, 36(1): 25-32.

链接本文:

http://www.sysydz.net/CN/10.11781/sysydz201401025      或      http://www.sysydz.net/CN/Y2014/V36/I1/25

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