塔中隆起中-下奥陶统岩溶水文地貌条件及控储机制

doi:10.7623/syxb201809004

石油学报 ›› 2018, Vol. 39 ›› Issue (9): 990-1005.DOI: 10.7623/syxb201809004

塔中隆起中-下奥陶统岩溶水文地貌条件及控储机制

张恒^1,2, 蔡忠贤^1,2, 漆立新³, 云露³, 曹自成³, 沙旭光³

1. 中国地质大学构造与油气资源教育部重点实验室湖北武汉 430074;
2. 中国地质大学资源学院湖北武汉 430074;
3. 中国石油化工股份有限公司西北油田分公司新疆乌鲁木齐 830011

收稿日期:2018-02-22 修回日期:2018-06-20 出版日期:2018-09-25 发布日期:2018-09-28
通讯作者: 蔡忠贤,男,1963年8月生,1985年获武汉地质学院学士学位,1999年获中国地质大学(北京)博士学位,现为中国地质大学(武汉)资源学院石油工程系教授,主要从事碳酸盐岩储层地质学研究。Email:zxcai@cug.edu.cn
作者简介:张恒,男,1988年11月生,2011年获中国地质大学(武汉)学士学位,2016年获中国地质大学(武汉)博士学位,现为中国地质大学(武汉)博士后,主要从事岩溶地质学、碳酸盐岩储层地质学和油藏描述研究。Email:cughzhang@163.com
基金资助:
中国科学院战略性先导科技专项（A类）（No.XDA14010302）和构造与油气资源教育部重点实验室开放基金课题（No.TPR-2014-19和No.TPR-2017-05）资助。

Hydrogeomorphological condition and its control mechanism on Mid-Lower Ordovician paleo-karst reservoirs,Tazhong uplift

Zhang Heng^1,2, Cai Zhongxian^1,2, Qi Lixin³, Yun Lu³, Cao Zicheng³, Sha Xuguang³

1. Key Laboratory of Tectonics and Petroleum Resources of Ministry of Education, China University of Geosciences, Hubei Wuhan 430074, China;
2. Faculty of Earth Resources, China University of Geosciences, Hubei Wuhan 430074, China;
3. Sinopec Northwest Oil Field Company, Xinjiang Urumqi 830011, China

Received:2018-02-22 Revised:2018-06-20 Online:2018-09-25 Published:2018-09-28

摘要/Abstract

摘要：

塔里木盆地塔中隆起中-下奥陶统古岩溶储层是深层碳酸盐岩油气勘探的重点目标。基于地震数据分析和地震属性提取，对塔中隆起的岩溶古地貌和古水文结构进行了精细刻画；通过钻井和成像测井对比、岩心和岩石学薄片观察，揭示了古岩溶储层空间分布的差异性；探讨了水文地貌条件对储层发育的控制作用。研究结果表明：①塔中隆起的中央主垒带位于古地形平坦的岩溶高地，发育以裂隙-扩散流为代表的流场结构；北斜坡带位于地势相对陡的岩溶斜坡，有利于形成顺层-径流的水流样式。②中央主垒带储层以裂缝-孔洞系统为主，为表层岩溶带的产物，其平面分布受控于NE和NWW向断裂；北斜坡带发育规模不一的孤立洞穴和多层溶蚀孔洞，其岩溶垂向结构相对完整。③由于水文地貌条件的差异，中央主垒带和北斜坡带分别形成了"裂隙-渗流"和"顺层-径流"表生岩溶储层发育模式，为储层预测提供了理论依据。

关键词: 表生岩溶, 水文地貌条件, 裂缝-孔洞系统, 岩溶储层发育模式, 中-下奥陶统, 塔中隆起, 塔里木盆地

Abstract:

Mid-Lower Ordovician paleo-karst reservoirs in the Tazhong uplift of Tarim Basin are the key targets of hydrocarbon exploration in deep-buried carbonate. Based on seismic volume analysis and seismic attribute extraction, the karst paleo-geomorphology and paleo-hydrological architecture of the Tazhong uplift were precisely delineated. Moreover, the variation in the spatial distribution of paleo-karst reservoirs was revealed by a correlation cross section of drilling and imaging logging, and core and thin-section petrological observations. Then the control effect of hydrogeomorphologic conditions on reservoir development was investigated in this study. The research results indicate that the central horst belt of the Tazhong uplift is located in karst highland with gentle paleo-terrain, where the flow field structure represented by fracture and diffuse flow is developed; the north-slope zone is located in karst slope with relatively steep terrain, which is beneficial for the formation of stratiform-runoff flow pattern. The reservoirs in the central horst zone are dominated by fissure-vug system produced in the epikarst zone, showing planar distribution controlled by NE and NWW-trending faults; the multi-layered corrosion vugs and isolated caves with different scales are developed in the north slope zone, showing a complete karst vertical structure. Because of the differences in hydrogeomorphologic conditions, the development patterns of "fissure-seepage" and "stratiform-runoff" epigenic karst reservoirs were established in the central horst zone and north slope zone respectively, providing theoretical references for reservoir prediction.

Key words: epigenic karst, hydrogeomorphologic condition, fissure-vug system, karst reservoir development pattern, Mid-Lower Ordovician, Tazhong uplift, Tarim Basin

中图分类号:

TE122.2

张恒, 蔡忠贤, 漆立新, 云露, 曹自成, 沙旭光. 塔中隆起中-下奥陶统岩溶水文地貌条件及控储机制[J]. 石油学报, 2018, 39(9): 990-1005.

Zhang Heng, Cai Zhongxian, Qi Lixin, Yun Lu, Cao Zicheng, Sha Xuguang. Hydrogeomorphological condition and its control mechanism on Mid-Lower Ordovician paleo-karst reservoirs,Tazhong uplift[J]. Acta Petrolei Sinica, 2018, 39(9): 990-1005.

参考文献

[1] JAMES N P,CHOQUETTE P W.Paleokarst[M].New York:Springer,1988.
[2] FRITZ R D,WILSON J L,YUREWICZ D A.Paleokarst related hydrocarbon reservoirs[M].SEPM Society for Sedimentary Geology,1993.
[3] LOUCKS R G.Paleocave carbonate reservoirs:origins,burial-depth modifications,spatial complexity,and reservoir implications[J].AAPG Bulletin, 1999,83(11):1795-1834.
[4] ZENG H L,LOUCKS R,JANSON X,et al.Three-dimensional seismic geomorphology and analysis of the Ordovician paleokarst drainage system in the central Tabei uplift,northern Tarim Basin,western China[J].AAPG Bulletin,2011,95(12):2061-2083.
[5] 付金华,白海峰,孙六一,等.鄂尔多斯盆地奥陶系碳酸盐岩储集体类型及特征[J].石油学报,2012,33(增刊2):110-117.
FU Jinhua,BAI Haifeng,SUN Liuyi,et al.Types and characteristics of the Ordovician carbonate reservoirs in Ordos Basin,China[J].Acta Petrolei Sinica,2012,33(S2):110-117.
[6] LOUCKS R G,MESCHER P K,MCMECHAN G A.Three-dimensional architecture of a coalesced,collapsed-paleocave system in the Lower Ordovician Ellenburger Group,central Texas[J].AAPG Bulletin,2004,88(5):545-564.
[7] TIAN Fei,JIN Qiang,LU Xinbian,et al.Multi-layered ordovician paleokarst reservoir detection and spatial delineation:a case study in the Tahe oilfield,Tarim Basin,Western China[J].Marine and Petroleum Geology,2016,69:53-73.
[8] ZHAO Wenzhi,SHEN Anjiang,QIAO Zhanfeng,et al.Carbonate karst reservoirs of the Tarim Basin,northwest China:types,features,origins,and implications for hydrocarbon exploration[J].Interpretation,2014,2(3):SF65-SF90.
[9] WRIGHT V P,BACETA J I,LAPOINTE P A.Paleokarstic macroporosity development at platform margins:lessons from the Paleocene of north Spain[J].Interpretation,2014,2(3):SF1-SF16.
[10] 李源,蔡忠贤.塔里木盆地塔河油田主体区海西早期岩溶台面划分及洞穴层对比[J].古地理学报,2016,18(4):560-568.
LI Yuan,CAI Zhongxian.Division of karst platform architecture and cave levels correlation in the early Hercynian,Tahe oilfield,Tarim Basin[J].Journal of Palaeogeography,2016,18(4):560-568.
[11] LU Xinbian,WANG Yan,TIAN Fei,et al.New insights into the carbonate karstic fault system and reservoir formation in the Southern Tahe area of the Tarim Basin[J].Marine and Petroleum Geology,2017,86:587-605.
[12] MYLROIE J E,MYLROIE J R,NELSON C S.Flank margin cave development in telogenetic limestone of New Zealand[J].Acta Carsologica,2008,37(1):15-40.
[13] WHITE W B.Science of caves and karst:a half century of progress[M]//FEINBERG J M,GAO Y L,ALEXANDER JR E C.Caves and karst across time.Boulder,Colorado:Geological Society of America Special Paper,2015,516:3.
[14] KLIMCHOUK A B,AULER A S,BEZERRA F H R,et al.Hypogenic origin,geologic controls and functional organization of a giant cave system in Precambrian carbonates,Brazil[J].Geomorphology,2016,253:385-405.
[15] 杨明德.岩溶峡谷区溶洞发育特征及水动力条件[J].贵州地质,1998,15(1):17-25.
YANG Mingde.Development of cavities in Karstic valley in respondent to hydodynamics[J].Guizhou Geology,1998,15(1):17-25.
[16] 梁虹,杨明德.喀斯特峰丛洼地(谷地)流域产汇流特性分析[J].贵州师范大学学报:自然科学版,1992,10(1):10-17.
LIANG Hong,YANG Mingde.Analysis of the characteristics of runoff-yield and flow-concentration in the drainage basin of the karst fengcong-depression district[J].Journal of Guizhou Normal University:Natural Sciences,1992,10(1):10-17.
[17] 闫福贵,梁永平,张翼龙,等.鄂尔多斯盆地周边地区岩溶发育模式及岩溶地下水开发利用探讨[J].地学前缘,2010,17(6):227-234.
YAN Fugui,LIANG Yongping,ZHANG Yilong,et al.Discussion about development mode of karst and exploitation of karst water around the Ordos Basin[J].Earth Science Frontiers,2010,17(6):227-234.
[18] PARISE M.Surface and subsurface karst geomorphology in the Murge (Apulia,Southern Italy)[J]. Acta Carsologica,2011,40(1):79-93.
[19] WHITE W B.Conceptual models for carbonate aquifers.1969[J].Ground Water,2012,50(2):180-186.
[20] FORD D C,WILLIAMS P W.Karst Hydrogeology and geomorphology[M].Chichester:Wiley,2007,562.
[21] 彭建,梁虹,王剑.贵州普定后寨河流域喀斯特水文地貌空间耦合分析[J].贵州师范大学学报:自然科学版,2000,18(2):1-5.
PENG Jian,LIANG Hong,WANG Jian.Karst hydro-geomorphological spatial coupling analysis of the Houzhaihe drainage area in Puding county,Guizhou province[J].Journal of Guizhou Normal University:Natural Science,2000,18(2):1-5.
[22] 王在高,徐萍莉.浅析喀斯特流域水文地貌过程-响应系统[J].贵州师范大学学报:自然科学版,2002,20(1):36-39.
WANG Zaigao,XU Pingli.An elementary analysis of hydro-geomorphological process-response system[J].Journal of Guizhou Normal University:Natural Science,2002,20(1):36-39.
[23] 杨明德,谭明,梁虹.喀斯特流域水文地貌系统[M].北京:地质出版社,1988.
YANG Mingde,TAN Ming,LIANG Hong.Hydrogeomorphologic system of karst drainage basin[M].Beijing:Geological Publishing House,1998.
[24] 张恒,蔡忠贤,漆立新,等.塔中地区西北部鹰山组成岩早期岩溶作用类型及其特征[J].石油与天然气地质, 2016,37(3):291-303.
ZHANG Heng,CAI Zhongxian,QI Lixin,et al.Types and characteristics of eogenetic karst in the Yingshan Formation in northwestern Tazhong area,Tarim Basin[J].Oil & Gas Geology,2016,37(3):291-303.
[25] 潘建国,卫平生,蔡忠贤,等.塔中地区中-下奥陶统碳酸盐岩孔洞-裂缝储集系统划分及其特征[J].地球科学-中国地质大学学报,2012,37(4):751-762.
PAN Jianguo,WEI Pingsheng,CAI Zhongxian,et al.Reservoir architectural system in the Middle-Lower Ordovician carbonate rock of Tazhong areas in Tarim[J].Earth Science-Journal of China University of Geosciences,2012,37(4):751-762.
[26] 倪新锋,沈安江,潘文庆,等.优质碳酸盐岩缝洞型储集层地质建模——以塔中北斜坡及塔北南缘奥陶系为例[J].石油勘探与开发,2013,40(4):414-422.
NI Xinfeng,SHEN Anjiang,PAN Wenqing,et al.Geological modeling of excellent fractured-vuggy carbonate reservoirs:a case study of the Ordovician in the northern slope of Tazhong palaeouplift and the southern area of Tabei slope,Tarim Basin[J].Petroleum Exploration and Development,2013,40(4):414-422.
[27] GAO Zhiqiang,LIU Zhongbao,GAO Shanlin,et al.Characteristics and genetic models of Lower Ordovician carbonate reservoirs in southwest Tarim Basin,NW China[J].Journal of Petroleum Science and Engineering,2016,144:99-112.
[28] 李阳,金强,钟建华,等.塔河油田奥陶系岩溶分带及缝洞结构特征[J].石油学报,2016,37(3):289-298.
LI Yang,JIN Qiang,ZHONG Jianhua,et al.Karst zonings and fracture-cave structure characteristics of Ordovician reservoirs in Tahe oilfield,Tarim Basin[J].Acta Petrolei Sinica,2016,37(3):289-298.
[29] 李源,鲁新便,王莹莹,等.塔河油田海西早期岩溶水文地貌特征及其演化[J].石油与天然气地质,2016,37(5):674-683.
LI Yuan,LU Xinbian,WANG Yingying,et al.Hydrogeomorphologic characterization and evolution of the Early Hercynian karstification in Tahe oilfield,the Tarim Basin[J].Oil & Gas Geology,2016,37(5):674-683.
[30] 李源,鲁新便,蔡忠贤,等.塔河油田海西早期古水文地貌特征及其对洞穴发育的控制[J].石油学报,2016,37(8):1011-1020.
LI Yuan,LU Xinbian,CAI Zhongxian,et al.Hydrogeomorphologic characteristics and its controlling caves in Hercynian,Tahe oilfield[J].Acta Petrolei Sinica,2016,37(8):1011-1020.
[31] 杨海军,韩剑发,孙崇浩,等.塔中北斜坡奥陶系鹰山组岩溶型储层发育模式与油气勘探[J].石油学报,2011,32(2):199-205.
YANG Haijun,HAN Jianfa,SUN Chonghao,et al.A development model and petroleum exploration of karst reservoirs of Ordovician Yingshan Formation in the northern slope of Tazhong palaeouplift[J].Acta Petrolei Sinica,2011,32(2):199-205.
[32] 冯仁蔚,欧阳诚,庞艳君,等.层间风化壳岩溶发育演化模式——以塔中川庆EPCC区块奥陶系鹰一段-鹰二段为例[J].石油勘探与开发,2014,41(1):45-54.
FENG Renwei,OUYANG Cheng,PANG Yanjun,et al.Evolution modes of interbedded weathering crust karst:a case study of the 1st and 2nd members of Ordovician Yingshan Formation in EPCC block,Tazhong,Tarim Basin[J].Petroleum Exploration and Development,2014,41(1):45-54.
[33] 张恒,蔡忠贤,漆立新,等.塔中隆起西北部中奥陶统一间房组地层识别对比及地质意义[J].石油学报,2017,38(6):622-635.
ZHANG Heng,CAI Zhongxian,QI Lixin,et al.Stratigraphic recognition and correlation of Middle Ordovician Yijianfang Formation in northwestern Tazhong uplift and its geological significances[J].Acta Petrolei Sinica,2017,38(6):622-635.
[34] FORD D C,WILLIAMS P W.Karst geomorphology and hydrology[M].London:Unwin Hyman,1989.
[35] WHITE W B,CULVER D C.Encyclopedia of caves[M].2nd ed.Waltham:Elsevier,2012:945.
[36] VERESS M.Karst environments:karren formation in high mountains[M].Netherlands:Springer,2010.
[37] WHITE W B.Geomorphology and hydrology of karst terrains[M].Oxford:Oxford University Press,1988.
[38] 孙崇浩,于红枫,王怀盛,等.塔里木盆地塔中地区奥陶系鹰山组碳酸盐岩孔洞发育规律研究[J].天然气地球科学,2012,23(2):230-236.
SUN Chonghao,YU Hongfeng,WANG Huaisheng,et al.Vugular formation of carbonates in Ordovician Yingshan reservoir in Tazhong northern slope of Tarim Basin[J].Natural Gas Geoscience,2012,23(2):230-236.
[39] 于靖波,李忠,杨柳,等.塔中北斜坡鹰山组深埋岩溶型储层刻画及分布规律[J].石油学报,2016,37(3):299-310.
YU Jingbo,LI Zhong,YANG Liu,et al.Characterization and distribution of deeply-buried paleokarst carbonate reservoirs of Ordovician Yingshan Formation in northern slope of central Tarim Basin[J].Acta Petrolei Sinica,2016,37(3):299-310.
[40] 江茂生,朱井泉,陈代钊,等.塔里木盆地奥陶纪碳酸盐岩碳、锶同位素特征及其对海平面变化的响应[J].中国科学:D辑,2002,32(1):36-42.
JIANG Maosheng,ZHU Jingquan,CHEN Daizhao,et al.Carbon and strontium isotope variations and responses to sea-level fluctuations in the Ordovician of the Tarim Basin[J].Science in China Series D:Earth Science,2001,44(9):816-823.
[41] 刘存革,李国蓉,朱传玲,等.塔河油田中下奥陶统岩溶缝洞方解石碳、氧、锶同位素地球化学特征[J].地球科学-中国地质大学学报,2008,33(3):377-386.
LIU Cunge,LI Guorong,ZHU Chuanling,et al.Geochemistry characteristics of carbon,oxygen and strontium isotopes of calcites filled in Karstic fissure-cave in lower-middle Ordovician of Tahe oilfield,Tarim Basin[J].Earth Science-Journal of China University of Geosciences,2008,33(3):377-386.

塔中隆起中-下奥陶统岩溶水文地貌条件及控储机制

Hydrogeomorphological condition and its control mechanism on Mid-Lower Ordovician paleo-karst reservoirs,Tazhong uplift

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