长岭断陷火山岩储层形成及控藏作用

徐宏节; 陆建林; 于文修; 王保华

doi:10.11781/sysydz201103239

长岭断陷火山岩储层形成及控藏作用

doi: 10.11781/sysydz201103239

1.
中国石化东北油气分公司, 长春130062
2. 中国石油化工股份有限公司石油勘探开发研究院无锡石油地质研究所, 江苏无锡214151

详细信息

作者简介:
徐宏节(1964- ),男,博士,高级工程师,从事石油地质综合研究及科研管理工作.E-mail:ssmonkey@vip.sina.com.

中图分类号: TE122.2⁺22
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出版历程
- 收稿日期: 2011-03-28
- 修回日期: 2011-05-27
- 刊出日期: 2011-06-28

Formation of volcanic reservoir and its controlling on accumulation in Changling Fault Depression

1.
Northeast Branch Company, SINOPEC, Changchun, Jilin 130062, China
2. Wuxi Research Institute of Petroleum Geology, SINOPEC, Wuxi, Jiangsu 214151, China

摘要

摘要: 长岭断陷火山岩厚度大,岩石类型多,相态类型齐全,储层发育。火山岩储层不受埋深限制,在深断陷具有良好储集能力,高孔低渗、低孔高渗特色明显;储集空间类型以气孔、溶蚀孔隙及与裂缝的组合为主,裂缝的存在改善了储层的渗流能力;储层类型以双孔双渗为主,少数具有似均质渗流等特征。火山岩优质储层的形成受多重因素控制,有利相带是火山岩储层发育的基础,构造运动是储层形成的关键,风化淋滤及溶解作用是优质储层形成的重要条件。发育在断裂带附近构造高部位的火山机构成藏条件较为有利。
- 火山岩 /
- 火山岩相 /
- 储层特征 /
- 控藏作用 /
- 长岭断陷
Abstract: In the Changling Fault Depression,volcanic rock formation is very thick.There are various types and facies of rock.Reservoirs are well-developed.The storage capacity of volcanic reservoir is not restricted by burial depth.It is favorable for reservoir in deep fault depression,characterized by high porosity and low permeability or low porosity and high permeability.Reservoir space is mainly composed of bubble pore,solution pore,fissure and their combination.Fissures improve the seepage ability of reservoir."Double porosities and double permeabilities" is the main reservoir type.Some reservoirs have homogeneous porosity and permeability.The formation of good volcanic reservoir is controlled by multiple factors.Favorable facies belt is the foundation.Tectonic movement is the key.Weathering leaching and dissolving also play important roles.The volcanic reservoirs near to the high position of tectonic fault are favorable for accumulation.
- volcanic rock /
- volcanic facies /
- reservoir characteristics /
- accumulation-controlling effect /
- Changling Fault Depression

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参考文献(11)

[1]	王德喜,陆建林.长岭断陷东部地区火山岩形成的构造控制作用研究[J].石油实验地质,2010,32(2):115-119.
[2]	秦伟军,郭金瑞.松辽盆地南部断陷层油气勘探领域[J].石油实验地质,2010,32(4):326-329.
[3]	吴群,周荔青.松辽盆地长岭断陷东部大中型火山岩(油)气田形成分布特征[J].石油实验地质,2009,31(1):40-45.
[4]	谢忱,胡纯心.松辽盆地长岭断陷南部天然气成藏与富集特征[J].石油与天然气地质,2010,31(3):381-385.
[5]	王大华,肖永军,徐佑德,等.松南长岭断陷查干花地区火山岩储层特征及影响因素[J].油气地质与采收率,2010,17(6):39-42.
[6]	张玉明,陆建林,李瑞磊,等.盆地油气储层研究中的火山岩岩相划分探讨[J].石油实验地质,2010,32(6):532-535.
[7]	杨双玲,刘万洙,于世泉,等.松辽盆地火山岩储层储集空同特征及其成因[J].吉林大学学报(地球科学版),2007,37(3):506-512.
[8]	陆建林,张玉明,徐宏节,等.松辽盆地长岭断陷火山岩储层形成特征研究[J].石油实验地质,2009,31(5):441-448.
[9]	赵海玲,黄微,王成,等.火山岩中脱玻化作用及其对储层的贡献[J].石油与天然气地质,2009,30(1):47-58.
[10]	闫林,周雪峰,高涛,等.徐深气田兴城开发区火山岩储层发育控制因素分析[J].大庆石油地质与开发,2007,26(2):9-13.
[11]	刘为付.松辽盆地徐家围子断陷深层火山岩储层特征及有利区预测[J].石油与天然气地质,2004,25(1):115-119.