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天然气地球科学 ›› 2011, Vol. 22 ›› Issue (6): 982–988.doi: 10.11764/j.issn.1672-1926.2011.06.982

• 天然气地质学 • 上一篇    下一篇

塔里木盆地奥陶系碳酸盐岩“非串珠状”缝洞型储层类型及成因

 王洪求, 刘伟方, 郑多明, 敬兵, 董瑞霞, 张喜梅, 李胜军   

  1. 1.中国石油勘探开发研究院西北分院，甘肃 兰州 730020;
    2.中国石油塔里木油田分公司勘探开发研究院，新疆 库尔勒 841000
  • 收稿日期:2011-08-17 修回日期:2011-10-23 出版日期:2011-12-10 发布日期:2011-12-10
  • 通讯作者: 王洪求wanghongqiu@petrochina.com.cn. E-mail:wanghongqiu@petrochina.com.cn.
  • 作者简介:王洪求(1982-)，男，湖北黄冈人,工程师,硕士,主要从事碳酸盐岩地震解释和储层预测方面的工作.E-mail:wanghongqiu@petrochina.com.cn.
  • 基金资助:

    国家科技重大专项大型油气田及煤层气开发项目“海相碳酸盐岩储层地震预测、油气藏描述技术研究”(编号：2011ZX05004-003)资助.

Types and Causes of “None string Beads” Fracture-cavity Reservoirs  in Ordovician Carbonate of Tarim Basin

WANG  Hong-Qiu, LIU  Wei-Fang, ZHENG  Duo-Ming, JING  Bing, DONG  Rui-Xia, ZHANG  Xi-Mei, LI  Sheng-Jun   

  1. 1. Northwest Research of Research Institute of Petroleum Exploration and Development,PetroChina,Lanzhou 730020,China;
    2.Research Institute of Exploration and Development, Tarim Oilfield Company,Korla 841000,China
  • Received:2011-08-17 Revised:2011-10-23 Online:2011-12-10 Published:2011-12-10

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摘要：

塔里木盆地奥陶系碳酸盐岩中“非串珠状”缝洞型储层经钻探已取得较好效果，但目前针对其储层类型及成因的研究较少。根据碳酸盐岩缝洞储集体发育程度及受风化壳和裂缝的影响程度，将在地震剖面上表现为“非串珠状”反射的缝洞型储层划分为3种类型，分别是内幕缝洞体规模较小的缝洞型储层、距风化壳较近的缝洞型储层以及裂缝型储层，进行正演模拟，并与实钻资料结合，详细探讨各自的地震反射特征和地质成因。

关键词: 碳酸盐岩, “非串珠状”缝洞型储层, 裂缝, 古河道, 塔里木盆地

Abstract:

Drilling of “none-string beads” fracture\|cavity reservoir has got a good effect in the Ordovician carbonate of Tarim basin, but the research about type and cause of the reservoir is not yet enough till now. Based on developing degree of cave-cleft bodies and influence of weathering crust and fracture, “none-string beads” fracture-cavity reservoirs in seismic section reflection are divided into three types, including reservoir with small scale inner cave\|cleft bodies, reservoir closer to weathering crust and fracture reservoir. Combining forward modeling with real drilling data, this paper discusses seismic reflection feature and geological genesis of each reservoir type in detail.

Key words: Carbonate reservoir, “None-string beads&rdquo, fracture-cavity reservoir, Fracture, Paleochannel, Tarim basin.

中图分类号: 

  • TE122.2


［1］Zhou Xinyuan,Wang Zhaoming,Liang Digang,et al.Tarim  Petroleum Exploration［M］.Beijing:Petroleum Industry Press,2009:14.［周新源,王招明,梁狄刚,等.塔里木油气勘探20年［M］.北京:石油工业出版社,2009:14.］
［2］Hu Zhongping.Mechanism and distinction method for the seismic“string beads”characteristic［J］.West  China  Petroleum  Geoscience,2006,2(4):423-426.［胡中平.溶洞地震波“串珠状”形成机理及识别方法［J］.中国西部油气地质,2006,2(4):423-426.］
［3］Yao Yao,Tang Wenbang.The oretical study of detectable cavern fractured reservoir in weathered karst of deer carbonatite［J］.Oil Geophysical Prospecting,2003,38(6):623-629.［姚姚,唐文榜.深层碳酸盐岩岩溶风化壳洞缝型油气藏可检测性的理论研究［J］.石油地球物理勘探,2003,38(6):623-629.］
［4］Sun Dong,Pan Jianguo,Yong Xueshan,et al.Formation  mechanism  of vertical “long string beads”in carbonate reservoir［J］.Oil Geophysical Prospecting,2010,45(supplementⅠ):101-104.［孙东,潘建国,雍学善,等.碳酸盐岩储层垂向长串珠形成机制［J］.石油地球物理勘探,2010,45(增刊Ⅰ):101-104.］
［5］Yang Ping.Study on Beadlike Reflections of Carbonate Reservoir in Ha6 3D Area［D］.  Beijing:China University of Petroleum(Beijing),2010:48-50.［杨平.哈6三维区碳酸盐岩储 层“串珠状反射”研究［D］.北京:中国石油大学(北京),2010:48-50.］
［6］Zhao Qun,Qu Shouli,Xue Shigui,et al.Study on the seismic response characteristics on the physical model of  carbonate  cave［J］.Geophysical Prospecting for Petroleum,2010,49(4):351-358.［赵群,曲寿利,薛诗桂,等.碳酸盐岩溶洞物理模型地震响应特征研究［J］.石油物探,2010,49(4):351-358.］
[JP]
［7］Yang Fengli,Wu Jianxun,Dong Liangguo.Seismic forward modeling and its response of dolomite  peleokarst reservoir in Tazhong  area of China［J］.Journal of Tongji University:Natural Science,2008,53(12):1724-1729.［杨风丽,吴建勋,董良国.塔中白云岩岩溶储层地震正演模拟及其响应［J］.同济大学学报:自然科学版,2008,53(12):1724-1729.］
［8］Wang Xiwen,Gao Jianhu,Liu Weifang,et al.Seismic  Prospecting  Application  in Complex  Regions［M］.Beijing:Petroleum Industry Press,2010:148.［王西文,高建虎,刘伟方,等.复杂地区地震勘探实践［M］.北京:石油工业出版社,2010:148.］
［9］Gu Jiayu,Zhu Xiaomin,Jia Jinhua.Sedimentology and Reservoir in Tarim Basin［M］.Beijing:Petroleum Industry Press,2003:147-148.［顾家裕,朱筱敏,贾进华.塔里木盆地沉积与储层［M］.北京:石油工业出版社,2003:147-148.］
［10］Sa Liming,Yao Fengchang,Di Bangrang,et al.Seismic response characteristics and identification method of fracture-cavity reservoir［J］.Lithologic Reservoirs,2011,23(1):23-28.［撒利明,姚逢昌,狄帮让,等.缝洞型储层地震响应特征与识别方法［J］.岩性油气藏,2011,23(1):23-28.］
［11］Ji Min,Wei Jianxin,Wang Shangxu.Analysis of seismic response  of  pore-cave physical model data［J］.Oil Geophysical Prospecting,2009,44(2):196-200.［季敏,魏建新,王尚旭.孔洞物理模型数据的地震响应特征分析［J］.石油地球物理勘探,2009,44(2):196-200.］
［12］Tang Wenbang,Liu Laixiang,Fan Jiafang,et al.Analytic technique of frequency difference for discrimination of cavity fillers［J］.Oil  &  Gas Geology,2002,23(1):41-44.［唐文榜,刘来祥,樊佳芳,等.溶洞充填物判识的频率差异分析技术［J］.石油与天然气地质,2002,23(1):41-44.］
［13］He Zhenhua,Du Zhengcong,Wen Xiaotao.Seismic modeling and predication of carbonate karst caves and fracture sets［J］.Advance in Earth Science,2004,19(3):399-402.［贺振华,杜正聪,文晓涛.碳酸盐岩喀斯特溶洞和裂缝系统的地震模拟与预测［J］.地球科学进展,2004,19(3):399-402.］
［14］Handford Robertson C.Modern Cave Systems as Analogs for Paleokarst Reservoirs:Part 1-Origin,Geometry,and Facies of Modern Systems; Part 2-Insights From Seismic Modeling［C］.Beijing:Ancient Karst Reservoirs Symposium,2004.
［15］Charlie Kerans.Carbonate Depositional Systems and Sequence Stratigraphy for Reservoir Characterization［C］.Huston:Carbonate Seminar of  BGP, 2008.
［16］Wang Huanhuan,Zhu Guangyou,Xue Haitao,et al.Formation and controlling factors of effective weathered crust carbonate reservoirs:Taking the Yingmaili-Yaha area of Tarim basin as an example［J］.Natural Gas Geoscience,2009,20(2):182-189.［王欢欢,朱光有,薛海涛,等.碳酸盐岩风化壳型有效储层的形成与控制因素研究——以塔里木盆地英买力—牙哈地区为例［J］.天然气地球科学,2009,20(2):182-189.］
［17］Teng Tuanyu,Cui Haifeng,Zhang Nianchun,et al.Prediction of fractured carbonate reservoirs using seismic data:An example of Yaha area in Tarim oilfield［J］.Natural Gas Geoscience,2009,20(2):270-272.［滕团余,崔海峰,张年春,等.碳酸盐岩裂缝储层地震预测技术——以牙哈地区为例［J］.天然气地球科学,2009,20(2):270-272.］
［18］Wang Fuhuan,Wang Zhaoming,Han Jianfa,et al.Geological conditions  of  oil and  gas enrichment in carbonate reservoirs of Tazhong  area,Tarim basin［J］.Natural Gas Geoscience,2009,20(5):695-701.［王福焕,王招明,韩剑发,等.塔里木盆地塔中地区碳酸盐岩油气富集的地质条件［J］.天然气地球科学,2009,20(5):695-701.］
［19］Zheng Xingping,Shen Anjiang,Shou Jianfeng,et al.A quantitative  plate  of  collapsed karst cave depth and its application in geological prediction and evaluation of carbonate reservoir［J］.Marine Origin Petroleum Geology,2009,17(4):55-59.［郑兴平,沈安江,寿建峰,等.埋藏岩溶洞穴垮塌深度定量图版及其在碳酸盐岩缝洞型储层地质评价预测中的意义［J］.海相油气地质,2009,17(4):55-59.］
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