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松辽盆地徐家围子断陷深层天然气含气系统与成藏机制
引用本文:王树学,周庆华,周庆强,李博,周建忠,赵轶林.松辽盆地徐家围子断陷深层天然气含气系统与成藏机制[J].天然气地球科学,2007,18(3):394-398.
作者姓名:王树学  周庆华  周庆强  李博  周建忠  赵轶林
作者单位:1. 吉林大学地球科学学院,吉林,长春,130061;大庆油田有限责任公司地质录井分公司,黑龙江,大庆,163411
2. 大庆油田有限责任公司地质录井分公司,黑龙江,大庆,163411
3. 大庆油田有限责任公司第八采油厂,黑龙江,大庆,163519
4. 大庆油田有限责任公司第二采油厂,黑龙江,大庆,163414
摘    要:通过对地质条件的研究,将松辽盆地徐家围子断陷深层划分为沙河子组和营城组-登二段、登二段-泉一段和泉二段、沙河子组和营城组-泉一段、泉二段3个含气系统,指出这3个含气系统形成于不同时期,其形成时期和演化对天然气运聚成藏和成藏模式有控制作用,认为该区深层天然气成藏与分布的主控因素是气源、盖层、断层和不整合面。

关 键 词:含气系统  天然气  深层  成藏机制  徐家围子断陷
文章编号:1672-1926(2007)03-0394-05
收稿时间:2007-03-07
修稿时间:2007-03-072007-04-25

GAS-BEARING SYSTEM AND ACCUMULATION MECHANISM OF DEEP LAYER IN XUJIAWEIZI FAULT DEPRESSION
WANG Shu-xue,ZHOU Qing-hua,ZHOU Qing-qiang,LI Bo,ZHOU Jian-zhong,ZHAO Yi-lin.GAS-BEARING SYSTEM AND ACCUMULATION MECHANISM OF DEEP LAYER IN XUJIAWEIZI FAULT DEPRESSION[J].Natural Gas Geoscience,2007,18(3):394-398.
Authors:WANG Shu-xue  ZHOU Qing-hua  ZHOU Qing-qiang  LI Bo  ZHOU Jian-zhong  ZHAO Yi-lin
Affiliation:1. School of Earth Sciences, Jilin University, Changchun 130061, China ; 2. Geological Logging Subcompany of Daqing Oilfield Company Ltd. , Daqing 163411, China; 3. No. 8 Oil Production Company of Daqing Oilfield Company Ltd. , Daqing 163519, China; 4. No. 2 Oil Production Company of Daqing Oilfield Company Ltd. , Daqing 163414, China
Abstract:By a study on source rocks and their space distribution characteristics,the deep layer in the Xujiaweizi fault depression is divided into three gas-bearing systems,which are K1sh+yc-K1d2,K1d2-K1q1+2 and K1sh+yc-K1q1+2.The main controlling factors of the deep gas reservoir forming are gas resource rock,cap rock,fault,and unconformity surface.Three gas-bearing systems of the Xujiaweizi fault depression are formed in different periods.There are four reservoir forming patterns.The accumulation periods and forming patterns of gas are controlled by the formation and evolvement periods of the gas-bearing systems.
Keywords:Gas-bearing system  Natural gas  Deep layer  Accumulation mechanism  Xujiaweizi fault depression  
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