Controlling factors for deep fluid activity and prediction of positive effect area in middle Tarim and Bachu regions

Meng Qingqiang; Zhu Dongya; Xie Qilai; Jin Zhijun

doi:10.11781/sysydz201106597

Volume 33 Issue 6

Turn off MathJax

Article Contents

Article Navigation > PETROLEUM GEOLOGY & EXPERIMENT > 2011 > 33(6): 597-601

Meng Qingqiang, Zhu Dongya, Xie Qilai, Jin Zhijun. Controlling factors for deep fluid activity and prediction of positive effect area in middle Tarim and Bachu regions[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2011, 33(6): 597-601. doi: 10.11781/sysydz201106597

Citation:

Meng Qingqiang, Zhu Dongya, Xie Qilai, Jin Zhijun. Controlling factors for deep fluid activity and prediction of positive effect area in middle Tarim and Bachu regions[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2011, 33(6): 597-601. doi: 10.11781/sysydz201106597

Citation:

PDF( 4310 KB)

Controlling factors for deep fluid activity and prediction of positive effect area in middle Tarim and Bachu regions

doi: 10.11781/sysydz201106597

1.
SINOPEC Exploration & Production Research Institute, Beijing 100083, China
2. College of Energy Resource, China University of Geosciences, Beijing 100083, China
3. College of Resource and Environment, South China University of Agriculture, Guangzhou, Guangdong 510640, China

Received Date: 2010-11-11
Rev Recd Date: 2011-11-06
Publish Date: 2011-12-28

Abstract

Abstract

Volcanic activities and deep faults caused deep fluid activities in the Tarim Basin.Volcanic activities gave birth to deep fluids,and deep faults provided pathways for deep fluids to migrate upwards.In the middle Tarim and Bachu regions,Permian volcanic rocks were widespread.Around well Zhong1 of the middle Tarim region and in faults such as Tumuxiuke,Selibuya,Kangtakumu and Mazhatage of Bachu region,volcanic activities were the most active.During the late Hercynian,the faults Tazhong Ⅰ,Tazhong well 10 and Tazhong Ⅱ in the middle Tarim region and the faults Tumuxiuke,Selibuya,Kangtakumu and Mazhatage in Bachu region were active faults for deep fluid activities.In this way,the middle Tarim and Bachu regions with active deep fluid were favorable for carbonate reservoir corrosion in the lower Paleozoic.
- volcanic activity,
- fault,
- deep fluid,
- reservoir corrosion,
- Bache region,
- middle Tarim region,
- Tarim Basin

FullText(HTML)

References(29)

References

[1]	金之钧,张刘平,杨雷,等.塔里木盆地深部流体的地球化学特征及油气成藏效应[J].地球科学——中国地质大学学报,2002,27(6):659-665.
[2]	杜乐天,王驹.气体地球化学:一个重要的研究方向[J].地球科学进展,1993,8(6):66-73.
[3]	毛景文,李晓峰.深部流体及其与成矿成藏关系研究现状[J].矿床地质,2004,23(4):520-532.
[4]	Luczaj J A,William B Harrison III,Williams N S.Fractured hydrothermal dolomite reservoirs in the Devonian Dundee Formation of the central Michigan Basin[J].AAPG Bulletin,2006,90(11):1787-1801.
[5]	Smith L B.Origin and reservoir characteristics of Upper Ordovician Trenton-Black River hydrothermal dolomite reservoirs in New York[J].AAPG Bulletin,2006,90(11):1691-1718.
[6]	Lavoie D,Morin C.Hydrothermal dolomitization in the lower Silurian Sayabec formation in northern Gaspé-Matapédia (Québec):constraint on timing of porosity and regional significance for hydrocarbon reservoirs[J].Bulletin of Canadian Petroleum Geology,2004,52(3):256-269.
[7]	Wilkinson J J,Earls G.A high temperature hydrothermal origin for black dolomite matrix breccias in the Irish Zn-Pb orefield[J].Mineralogical Magazine,2000,64(6):1017-1036.
[8]	Navon O,Hutcheon I D,Rossman G R.Mantle-derived fluids in diamond micro-inclusions[J].Nature,1988,335:784-789.
[9]	Bell D R,Rossman G R.Water in Earth's mantle:the role of no-minally anhydrous minerals[J].Science,1992,255:1391-1397.
[10]	路凤香.深部地幔及地幔流体[J].地学前缘,1996,3(3-4):181-185.
[11]	张铭杰,王先彬,李立武.地幔流体组成[J].地学前缘,2000,7(2):401-412.
[12]	Hu Wenxuan,Jin Zhijun,Song Yucai,et al.Theoretical Calculation model of heat transfer for deep-derived supercri-tical fluids with a case study[J].Acta Geologica Sinica,2004,78(1):221-229.
[13]	Wierzbicki R,Dravis J J,Al-Aasm I,et al.Burial dolomitization and dissolution of Upper Jurassic Abenaki platform carbonates,Deep Panuke reservoir,Nova Scotia,Canada[J].AAPG Bulletin,2006,90(11):1843-1861.
[14]	Lavoie D,Chi G,Brennan-Alpert P,et al.Hydrothermal dolomitization in the lower Ordovician Romaine formation of the Anticosti basin:significance for hydrocarbon exploration[J].Bulletin of Canadian Petroleum Geology,2005,53(4):454-472.
[15]	Malone M J,Baker P A,Burns S T.Hydrothermal dolomitization and recrystallizationg of dolomite breccias from the Miocene Monterey formation,Tepusquet aera,California[J].Journal of Sedimentary Research,1996,66(5):976-990.
[16]	金之钧,朱东亚,胡文瑄,等.塔里木盆地热液活动地质地球化学特征及其对储层影响[J].地质学报,2006,80(2):245-253.
[17]	吕修祥,杨宁,解启来,等.塔中地区深部流体对碳酸盐岩储层的改造作用[J].石油与天然气地质,2005,26(3):284-289,296.
[18]	朱东亚,金之钧,胡文瑄,等.塔里木盆地深部流体对碳酸盐岩储层的影响[J].地质论评,2008,54(3):348-354.
[19]	朱东亚,金之钧,胡文瑄.塔中地区热液改造型白云岩储层[J].石油学报,2009,30(5):698-704.
[20]	Zhu Dongya,Jin Zhujun,Hu Wenxuan.Hydrothermal recrystallization of the Lower Ordovician dolomite and its significance to reservoir in northern Tarim Basin[J].Science in China Series D:Earth Sciences,2010,53(3):368-381.
[21]	陈代钊.构造—热液白云岩化作用与白云岩储层[J].石油与天然气地质,2008,29 (5):614-622.
[22]	陈汉林,贾承造.塔里木盆地地质热事件研究[J].科学通报,1997,42(10):1096-1099.
[23]	贾承造,魏齐国,姚慧君.盆地构造演化和区域构造地质[M].北京:石油工业出版社,1995.
[24]	贾承造.中国塔里木盆地构造特征与油气[M].北京:石油工业出版社,1997:37.
[25]	李曰俊,苏文,杨树春,等.塔中—巴楚地区断裂系统、火成岩及其对油气的控制作用.乌鲁木齐:中国石化西部新区勘探指挥部,2005:46-61.
[26]	张仲培,郑孟林,周波,等.塔里木盆地巴楚地区勘探潜力与目标评价.北京:中国石化股份有限公司,2008:23-35.
[27]	赵锡奎,何建军,张小兵,等.阿克库勒凸起构造演化与古构造研究.乌鲁木齐:中国石化西北油田分公司勘探开发研究院,2009:33-41.
[28]	张仲培,郑孟林,周波,等.塔里木盆地巴楚地区勘探潜力与目标评价.北京:中国石化股份有限公司,2008:23-35.
[29]	李曰俊,吴根耀,孟庆龙,等.塔里木西部地区古生代断裂活动的方式和机制[J].地质科学,2008,43 (4):727-745.

Relative Articles

Supplements(0)

Cited By

Proportional views

Proportional views

通讯作者: 陈斌, bchen63@163.com

1.
沈阳化工大学材料科学与工程学院沈阳 110142

Citation

XML

PDF-CN

Article Metrics

Article views (3355) PDF downloads(964)

Controlling factors for deep fluid activity and prediction of positive effect area in middle Tarim and Bachu regions

doi: 10.11781/sysydz201106597

Abstract

References

Proportional views

Catalog

通讯作者: 陈斌, bchen63@163.com

Article Metrics

Proportional views

Related

Controlling factors for deep fluid activity and prediction of positive effect area in middle Tarim and Bachu regions

doi: 10.11781/sysydz201106597

Abstract

References

Proportional views

Catalog

通讯作者: 陈斌, bchen63@163.com

Article Metrics

Proportional views

Related

Export File

Citation

Format

Content