Carbonate Reservoir Rock of Composite Genesis and Its Dynamic Developing Process:An Example from Tahe Carbonate Reservoir

ZHU Dong-Ya, MENG  Qing-Qiang, JIN  Zhi-Jun, HU  Wen-Xuan

doi:10.11764/j.issn.1672-1926.2012.01.26

2012 , Vol. 23 >Issue 1: 26 - 35

DOI: https://doi.org/10.11764/j.issn.1672-1926.2012.01.26

Carbonate Reservoir Rock of Composite Genesis and Its Dynamic Developing Process:An Example from Tahe Carbonate Reservoir

Expand

1.Laboratory of Structural and Sedimentological Reservoir Geology,Petroleum Production andResearch Institute of SINOPEC,Beijing 100083,China;
2.Department of Earth Sciences,Nanjing University,Nanjing 210093,China

Received date: 2011-05-17

Revised date: 2011-11-14

Online published: 2012-02-10

Fold

Abstract

The lower Paleozoic carbonate in the Tarim basin experienced many kinds of secondary dissolution,such as surface dissolution by atmospheric eluviation,burial dissolution by organic fluid,surface karst by meteoric water,hydrothermal alteration by magma-associated hydrothermal fluid,and so on.Taking the Tahe oilfield as an example,the Ordovician carbonates experienced three periods of strong surface karst at the middle Caledonian period in the west and north of Tahe oilfield,early Hercynian in the main block,and later Hercynian in the northwest part,respectively.Under the action of hydrocarbon-filling at the periods of Caledonian,later Hercynian and Himalayan,several time of burial dissolution were taken to the carbonates by organic fluid.The burial dissolution mainly developed to the south of the O₂yj distinction line,and the space of carbonate reservoir acted by burial dissolution was overlaid to the early-formed one.Since the extensive magmatic-volcanic activities at the later Hercynian period (Permian) made the deep hydrothermal active,the hydrothermal alteration dissolved the carbonates remarkably.The hydrothermal-dissolved pores stacked on the previously existing reservoir space in the west and southwest of the Tahe oilfield.Therefore,the high quality of carbonate reservoir was formed rather by one single fluid than the composition of multiple dissolutions in a long-time dynamic process.

Key words： Tarim basin; Carbonate; Burial dissolution; Surface karst; Hydrothermal dissolution; Dynamic developing.

Cite this article

ZHU Dong-Ya, MENG Qing-Qiang, JIN Zhi-Jun, HU Wen-Xuan . Carbonate Reservoir Rock of Composite Genesis and Its Dynamic Developing Process:An Example from Tahe Carbonate Reservoir[J]. Natural Gas Geoscience, 2012 , 23(1) : 26 -35 . DOI: 10.11764/j.issn.1672-1926.2012.01.26

References

［1］Wang Shuyi,Chen Qianglu,Ma Hongqiang.Burial corrasion of lower Ordovician carbonate rocks and its infuluence on reservoir in Tahe oilfield,Tarim basin［J］.Petroleum and Experiment Geology,2003,25(supplement):557-561.［王恕一,陈强路,马红强.塔里木盆地塔河油田下奥陶统碳酸盐岩的深埋溶蚀作用及其对储集体的影响［J］.石油实验地质,2003,25(增刊):557-561.］
［2］Zhang Tao,Yan Xiangbin,Wang Shuyi,et al.Characteristics and genesis of reef-bank facies reservoirs with dissolution pores in Ordovician Yijianfang Formation in Tahe oilfield［J］.Oil and Gas Geology,2004,25(4):462-466,471.［张涛,闫相宾,王恕一,等.塔河油田奥陶系一间房组礁滩相溶蚀孔隙型储层特征与成因［J］.石油与天然气地质,2004,25(4):462-466,471.］
［3］Zhao Zongju,Wang Zhaoming,Wu Xingning,et al.Genetic types and distribution forecast of available carbonate reservoirs in Ordovician in the central area of Tarim basin［J］.Petroleum Experiment Geology,2007,29(1):40-46.［赵宗举,王招明,吴兴宁,等.塔里木盆地塔中地区奥陶系储层成因类型及分布预测［J］.石油实验地质,2007,29(1):40-46.］
［4］Jin Zhijun,Zhu Dongya,Hu Wenxuan,et al.Mesogenetic dissolution of the middle Ordovician limestone in the Tahe oilfield of Tarim basin,NW China［J］.Marine and Petroleum Geology,2009,26(6):753-763.
［5］Yan Xiangbin.The paleo-karst of the lower Ordovician carbonate and reservoir characteristics in the Tahe oilfield［J］.Journal of Jianghan Petroleum Institute,2002,24(4):23-25.［闫相宾.塔河油田下奥陶统古岩溶作用及储层特征［J］.江汉石油学院学报,2002,24(4):23-25.］
［6］Yan Xiangbin,Li Tiejun,Zhang Tao,et al.Differences between formation conditions of Ordovician karstic reservoirs in Tazhong and Tahe areas［J］.Oil and Gas Geology,2005,26(2):202-207.［闫相宾,李铁军,张涛,等.塔中与塔河地区奥陶系岩溶储层形成条件的差异［J］.石油与天然气地质,2005,26(2):202-207.］
［7］Miao Jijun,Jia Chengzao,Zou Caineng,et al.Characteristics and exploration fields of plaeo-karst reservoirs at the top of early Ordovician in center Tarim uplift［J］.Nature Gas Geoscience,2007,18(4):497-500,606.［苗继军,贾承造,邹才能,等.塔中地区下奥陶统岩溶风化壳储层特征与勘探领域［J］.天然气地球科学,2007,18(4):497-500,606.］
［8］Chen Qianglu,He Zhiliang,Li Sitian.Hydrocarbon accumulation zones of Ordovician carbonate reservoir in Tazhong area of the Tarim basin［J］.Petroleum Geology and Experiment,2007,29(4):367-372.［陈强路,何治亮,李思田.塔中地区奥陶系碳酸盐岩储层与油气聚集带［J］.石油实验地质,2007,29(4):367-372.］
［9］Wang Simin,Jin Zhijun,Xie Qilai.Transforming effect of deep fluids on carbonate reservoirs in the well TZ45 region［J］.Geological Review,2004,50(5):543-547.［王嗣敏,金之钧,解启来.塔里木盆地塔中45井区碳酸盐岩储层的深部流体改造作用［J］.地质论评,2004,50(5):543-547.］
［10］Zhu Yixiu,Jin Zhijun,Lin Changsong.Relations between the early Permian magmatic rocks and hydrocarbon accumulation in the central Tarim［J］.Petroleum and Experiment Geology,2005,27(1):50-54,61.［朱毅秀,金之钧,林畅松.塔里木盆地塔中地区早二叠世岩浆岩及油气成藏关系［J］.石油实验地质,2005,27(1):50-54,61.］
［11］Zhu Dongya,Hu Wenxuan,Song Yucai,et al.Fluoritization in Tazhong 45 reservoir:Characteristics and its effect on the reservoir bed［J］.Acta Petrologica et Mineralogica,2005,24(3):205-215.［朱东亚,胡文瑄,宋玉才,等.塔里木盆地塔中45 井油藏萤石化特征及其对储层的影响［J］.岩石矿物学杂志,2005,24(3):205-215.］
［12］Jin Zhijun,Zhu Dongya,Hu Wenxuan,et al.Geological and geochemical signatures of hydrothermal activity and their influence on carbonate reservoir beds in the Tarim basin［J］.Acta Geologica Sinica,2006,80(2):245-253.［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的影响［J］.地质学报,2006,80(2):245-253.
［13］Qian Yixiong,Chen Yue,Chen Qianglu.General characteristics of burial dissolution for Ordovician carbonate reservoirs in the northwest of Tazhong area［J］.Acta Petrolei Sinica,2006,27(3):47-52.［钱一雄,陈跃,陈强路.塔中西北部奥陶系碳酸盐岩埋藏溶蚀作用［J］.石油学报,2006,27(3):47-52.］
［14］Zhu Dongya,Jin Zhijun,Hu Wenxuan,et al.Effects of deep fluid on carbonates reservoir in Tarim basin［J］.Geological Review,2008,54(3):348-354.［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影响［J］.地质论评,2008,54(3):348-354.］
［15］Zhu Dongya,Jin Zhijun,Hu Wenxuan.Hydrothermally altered dolomite reservoir in Tazhong area［J］.Acta Petrolei Sinica,2009,30(5):698-704.［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.］
［16］Wu Guanghui,Li Qiming,Xiao Zhongyao,et al.The evolution characteristics of palaeo-uplifts in Tarim basin and its exploration directions for oil and gas［J］.Geotectonica et Metallogenia,2009,33(1):124-130.［邬光辉,李启明,肖中尧,等.塔里木盆地古隆起演化特征及油气勘探［J］.大地构造与成矿学,2009,33(1):124-130.］
［17］Chen Ruiyin,Zhao Wenzhi,Zhang Shuichang,et al.The geological proofs on the hydrocarbon generation of and accumulation in the lower Paleozoic carbonate in the later period in the Tarim basin［J］.Earth Science Frontiers,2009,16(4):173-181.［陈瑞银,赵文智,张水昌,等.塔里木盆地下古生界油气晚期成烃成藏的地质依据［J］.地学前缘,2009,16(4):173-181.］
［18］Liu Luofu.Distribution and significance of the carbazole compounds in Palaeozoic oils from Tazhong uplift,Tarim basin［J］.Acta Geologica Sinica,1998,72(1):82-93.
［19］Liang Digang,Zhang Shuichang,Zhang Baomin,et al.On the petroleum generation from marine sedimentary in China,the evidences from the Tarim basin［J］.Earth Science Frontiers,2000,7(4):534-547.［梁狄刚,张水昌,张宝民,等.从塔里木盆地看中国海相生油问题［J］.地学前缘,2000,7(4):534-547.］
［20］Zhang Shuichang,Wang Feiyu,Zhang Baomin,et al.Middle-upper Ordovician source rock geochemistry of the Tarim basin［J］.Acta Petrolei Sinica,2000,21(6):23-28.［张水昌,王飞宇,张保民,等.塔里木盆地中—上奥陶统油源层地球化学研究［J］.石油学报,2000,21(6):23-28.］
［21］Zhang Shuichang,Zhang Baomin,Wang Feiyu,et al.Middle-upper Ordovician:The main source for hydrocarbon of Tarim basin［J］.Marine Petroleum Geology,2000,5(1/2):16-22.［张水昌,张宝民,王飞宇,等.中—上奥陶统：塔里木盆地主要油源层［J］.海相油气地质,2000,5(1/2):16-22.］
［22］Zhao Jingzhou.Evoluation on the Cambrian-Ordovician marine source rocks from the north Tarim basin［J］.Acta Sedimentologica Sinica,2001,19(1):117-124.［赵靖舟.塔里木盆地北部寒武—奥陶系海相烃源岩重新认识［J］.沉积学报,2001,19(1):117-124.］
［23］Yu Bingsong,Fan Tailiang.Sedimentary-tectonic control on the development of muddy hydrocarbon source rocks of Cambrian-Ordovician from Tarim basin［J］.Modern Geoscience,2008,22(4):534-540.［于炳松,樊太亮.塔里木盆地寒武系—奥陶系泥质烃源岩发育的构造和沉积背景控制［J］.现代地质,2008,22(4):534-540.］
［24］Liu Luofu,Zhao Jianzhang,Zhang Shuichang,et al.Origin and characteristics of the Silurian butimen sandstone in the Tarim basin［J］.Acta Petrolei Sinica,2000,21(6):12-17.［刘洛夫,赵建章,张水昌,等.塔里木盆地志留系沥青砂岩的成因类型及特征［J］.石油学报,2000,21(6):12-17.］
［25］Wu Guanghui,Chen Lixin,Xu Zhiming,et al.Mechanism of hydrocarbon pooling in the Ordovician carbonate reservoirs in Tazhong area of the Tarim basin［J］.Natural Gas Industry,2008,28(6):19-22.［邬光辉,陈利新,徐志明,等.塔中奥陶系碳酸盐岩油气成藏机理［J］.天然气工业,2008,28(6):19-22.］
［26］Zhang Nianchun,Cui Haifeng,Teng Tuanyu,et al.Features of carbonate buried hill oil and gas reservoir in Yingmaili-Yaha region,Tarim basin［J］.Natural Gas Geoscience,2010,21(5):762-771.［张年春,崔海峰,滕团余,等.塔里木盆地英买力—牙哈地区碳酸盐岩潜山油气藏特征研究［J］.天然气地球科学,2010,21(5):762-771.］
［27］Chen Hanlin,Yang Shufeng,Jia Chengzao,et al.Geological thermal events in Tarim basin［J］.Chinese Science Bulletin,1997,42(7):580-580.
［28］Jia Chengzao.The Tectonics Characteristics and Oil of Gas in the Tarim Basin in China［M］.Beijing:Petroleum Industry Press,1997:37.［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.］
［29］Mazzullo S J,Harris P M.Mesogenetic dissolution:Its role in porosity development in carbonate reservoir［J］.AAPG Bulletin,1992,76(5):607-620.
［30］Spirakis C S,Heyl A V.Possible effects of thermal degradation of organic matter on carbonate paragenesis and fluorite precipitation in Mississippi Valley-type deposits［J］.Geology,1988,16:1117-1120.
［31］Moore C H.Carbonate Diagenesis and Porosity［M］//Developments in Sedimentology.Amsterdam:Elsevier Science Ltd,1989:338.
［32］Yu Renlian,Fu Heng.Influence of tectonic movement on Ordovician carbonates of Tahe oilfield［J］.Natural Gas Exploration and Development,2006,29(2):1-6.［俞仁连,傅恒.构造运动对塔河油田奥陶系碳酸盐岩的影响［J］.天然气勘探与开发,2006,29(2):1-6.］
［33］Zhang Nai,Zhao Zongju,Xiao Zhongyao,et al.Characteristics of hydrocarbon fluid in the Ordovician vein calcite of Tazhong No.1 slope-break zone［J］.Natural Gas Geoscience,2010,21(3):389-396.［张鼐,赵宗举,肖中尧,等.塔中Ⅰ号坡折带奥陶系裂缝方解石烃包裹体特征及成藏［J］.天然气地球科学,2010,21(3):389-396.］
［34］Zhao Zongju,Zhou Xinyuan,Chen Xueshi,et al.Characteristics of paleo-karst reservoirs of middle-late Ordovician in Tazhong area,Tarim basin［J］.Xinjiang Petroleum Geology,2006,27(6):660-663.［赵宗举,周新源,陈学时,等.塔中地区中晚奥陶世古潜山岩溶储集层特征［J］.新疆石油地质,2006,27(6):660-663.］
［35］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):182-191.［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):182-191.］
［36］He Zhiliang,Peng Shoutao,Zhang Tao.Controlling factors and genetic pattern of the Ordovician reservoirs in the Tahe area，Tarim basin［J］.Oil and Gas Geology,2010,31(6):743-752.［何治亮,彭守涛,张涛.塔里木盆地塔河地区奥陶系储层形成的控制因素与复合-联合成因机制［J］.石油与天然气地质,2010,31(6):743-752.］
［37］Liu Yukui,Zheng Duoming,Wang Jianning,et al.The Ordovician reservoir characteristics and mineralization in Yingmaili low heave of Tarim basin［J］.Natural Gas Geoscience,2005,16(5):587-591.［刘玉魁,郑多明,王建宁,等.塔里木盆地英买力低凸起奥陶系碳酸盐岩储层特征及其成岩作用［J］.天然气地球科学,2005,16(5):587-591.］
［38］Ye Desheng,Wang Genchang,Lin Zhongmin.Characteristics of the Cambrian-Ordovician Carbonates and Prospect of Hydrocarbon Exploration in North of the Tarim Basin［M］.Chengdu:Press of Sichuan University,2000:88-147.［叶德胜，王根长，林忠民．塔里木盆地北部寒武—奥陶系碳酸盐岩特征及油气远景［M］.成都：四川大学出版社，2000:88-147.］

Options

Outlines

模态框（Modal）标题

Abstract

Cite this article

References