塔里木盆地中—下奥陶统岩溶水文地貌结构类型及特征

doi:10.7623/syxb202001004

石油学报 ›› 2020, Vol. 41 ›› Issue (1): 43-58.DOI: 10.7623/syxb202001004

塔里木盆地中—下奥陶统岩溶水文地貌结构类型及特征

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

1. 中国地质大学(武汉)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(武汉)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:2019-04-26 修回日期:2019-11-11 出版日期:2020-01-25 发布日期:2020-02-06
通讯作者: 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
作者简介: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
基金资助:
中国科学院战略性先导科技专项（A类）（XDA14010302）和构造与油气资源教育部重点实验室开放基金课题（TPR-2014-19，TPR-2017-05）资助。

Types and characteristics of karst hydrogeomorphologic architecture in the Middle-Lower Ordovician,Tarim Basin

Cai Zhongxian^1,2, Zhang Heng^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. School of Earth Resources, China University of Geosciences, Hubei Wuhan 430074, China;
3. Sinopec Northwest Oil Field Company, Xinjiang Urumqi 830011, China

Received:2019-04-26 Revised:2019-11-11 Online:2020-01-25 Published:2020-02-06

摘要/Abstract

摘要：

表生型岩溶储层是塔里木盆地中—下奥陶统油气勘探的重点目标。为了深入认识岩溶储层的分区差异性，基于塔里木盆地大量钻井、取心和地震资料以及柯坪地区野外露头考察资料，对塔里木盆地不同地区中—下奥陶统岩溶古地貌和古水文进行了精细刻画，并划分了岩溶水文地貌结构类型，揭示了水文地貌结构对岩溶储层发育的控制效应。研究结果表明：①塔里木盆地中—下奥陶统岩溶水文地貌结构可划分为地表—地下双重水系型、地表水系型和无地表水系型；②地表—地下双重水系型结构主要发育在石炭系覆盖区，其主要特征是岩溶水形成了丰富的岩溶地貌类型，并建立了完整的地表岩溶流域和综合性岩溶管道网络；③地表水系型结构主要出现在志留系覆盖区，其主要特征是岩溶水对地表岩溶地貌产生了重要改造，虽然形成了较为完善的地表水系，但尚未产生综合性岩溶排驱系统；④无地表水系型结构主要分布在上奥陶统覆盖区，其主要特征是岩溶水对可溶性地层尚未产生明显的切割改造，地表未形成清晰的水系网络；⑤塔里木盆地3种不同类型的水文地貌结构反映了不同的岩溶演化阶段，控制了不同地区呈巨大差异的中—下奥陶统表生岩溶储层。

关键词: 水文地貌结构, 岩溶古地貌, 岩溶古水文, 表生岩溶储层, 中—下奥陶统, 塔里木盆地

Abstract:

Epigenetic karst reservoir is the key target for oil and gas exploration in the Middle-Lower Ordovician of Tarim Basin. To deeply understand the zonal differences of karst reservoirs, based on plenty of drilling, coring and seismic data from the Tarim Basin and the investigation data of field outcrops from the Keping area, this paper meticulously describes the ancient paleo-geomorphology and paleo-hydrology of the Middle-Lower Ordovician in different areas of Tarim Basin, classifies the types of hydrogeomorphic architecture in karst zones and reveals the controlling effect of hydrogeomorphic architecture on the development of karst reservoirs. The results show that:(1) The Middle-Lower Ordovician hydrogeomorphic architecture in karst zones of Tarim Basin can be divided into three types, i.e., surface-underground dual drainage system, surface drainage system and non-surface drainage system. (2) The surface-underground dual drainage system is mainly developed in the area covered by the Carboniferous. Its main feature is that diverse types of karst landforms are formed by karst water, and a complete surface karst watershed and an integrated conduit system have been established. (3) The surface drainage system is mainly found in the area covered by the Silurian, and its main feature is that the surface karst landforms have been significantly transformed by karst water. Although a relatively complete surface drainage system has been formed, a comprehensive expulsion system in karst zones has not yet been established. (4) The non-surface drainage system is mainly distributed in the area covered by the Upper Ordovician. Its main feature is that soluble strata have not been significantly sculptured and transformed by karst water, and a clear network of water system has been formed. (5) Three different types of hydrogeomorphic architectures in Tarim Basin reflect different evolution stages of karst and control the development of Middle-Lower Ordovician spigenetic karst reservoirs, which have huge differences in different regions.

Key words: hydrogeomorphologic architecture, karst paleo-geomorphology, karst paleo-hydrology, epigenetic karst reservoirs, Middle-Lower Ordovician, Tarim Basin

中图分类号:

TE122.2

蔡忠贤, 张恒, 漆立新, 云露, 曹自成, 沙旭光. 塔里木盆地中—下奥陶统岩溶水文地貌结构类型及特征[J]. 石油学报, 2020, 41(1): 43-58.

Cai Zhongxian, Zhang Heng, Qi Lixin, Yun Lu, Cao Zicheng, Sha Xuguang. Types and characteristics of karst hydrogeomorphologic architecture in the Middle-Lower Ordovician,Tarim Basin[J]. Acta Petrolei Sinica, 2020, 41(1): 43-58.

参考文献

[1] 康玉柱.中国海相油气田勘探实例之四:塔里木盆地塔河油田的发现与勘探[J].海相油气地质,2005,10(4):31-38.
KANG Yuzhu.Cases of discovery and exploration of marine fields in China (Part 4):Tahe Oilfield in Tarim Basin[J].Marine Origin Petroleum Geology,2005,10(4):31-38.
[2] 周新源,杨海军,韩剑发,等.中国海相油气田勘探实例之十二:塔里木盆地轮南奥陶系油气田的勘探与发现[J].海相油气地质,2009,14(4):67-77.
ZHOU Xinyuan,YANG Haijun,HAN Jianfa,et al.Cases of discovery and exploration of marine fields in China (Part 12):Lunnan Ordovician oil-gas field in Tarim Basin[J].Marine Origin Petroleum Geology,2009,14(4):67-77.
[3] 朱光有,杨海军,朱永峰,等.塔里木盆地哈拉哈塘地区碳酸盐岩油气地质特征与富集成藏研究[J].岩石学报,2011,27(3):827-844.
ZHU Guangyou,YANG Haijun,ZHU Yongfeng,et al.Study on petroleum geological characteristics and accumulation of carbonate reservoirs in Hanilcatam area,Tarim Basin[J].Acta Petrologica Sinica,2011,27(3):827-844.
[4] 崔海峰,郑多明,李得滋.英买力地区碳酸盐岩内幕油气藏特征及勘探方向[J].石油地球物理勘探,2010,45(Z1):196-201.
CUI Haifeng,ZHENG Duoming,LI Dezi.Reservoir characteristics and exploration trend for carbonate inner reservoir in Yingmali area[J].Oil Geophysical Prospecting,2010,45(Z1):196-201.
[5] 韩剑发,韩杰,江杰,等.中国海相油气田勘探实例之十五:塔里木盆地塔中北斜坡鹰山组凝析气田的发现与勘探[J].海相油气地质,2013,18(3):70-78.
HAN Jianfa,HAN Jie,JIANG Jie,et al.Cases of discovery and exploration of marine fields in China,Part 15:Ordovician Yingshan condensate gas field in north slope of Tazhong uplift,Tarim Basin[J].Marine Origin Petroleum Geology,2013,18(3):70-78.
[6] 黄太柱.塔里木盆地玉北地区断裂系统解析[J].石油与天然气地质,2014,35(1):98-106.
HUANG Taizhu.Analysis on the fault system of Yubei region,Tarim Basin[J].Oil & Gas Geology,2014,35(1):98-106.
[7] 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.
[8] GAO Zhiqian,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 & Engineering,2016,144:99-112.
[9] 刘存革,徐明军,云露,等.塔里木盆地阿克库勒凸起奥陶系海西晚期古岩溶特征[J].石油实验地质,2015,37(3):280-285.
LIU Cunge,XU Mingjun,YUN Lu,et al.Characteristics of Late Hercynian paleokarsts in Akekule uplift,Tarim Basin[J].Petroleum Geology & Experiment,2015,37(3):280-285.
[10] 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.
[11] 罗春树,杨海军,李江海,等.塔中奥陶系优质储集层特征及断裂控制作用[J].石油勘探与开发,2011,38(6):716-724.
LUO Chunshu,YANG Haijun,LI Jianghai,et al.Characteristics of high quality Ordovician reservoirs and controlling effects of faults in the Tazhong area,Tarim Basin[J].Petroleum Exploration and Development,2011,38(6):716-724.
[12] 淡永,梁彬,张庆玉,等.塔北哈拉哈塘地区奥陶系碳酸盐岩浅覆盖区岩溶储层特征与形成机理[J].石油物探,2015,54(1):90-98.
DAN Yong,LIANG Bin,ZHANG Qingyu,et al.Characteristics and genesis of Ordovician carbonate karst reservoir in the shallow coverage zone of Halahatang area,northern Tarim Basin[J].Geophysical Prospecting for Petroleum,2015,54(1):90-98.
[13] 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.
[14] 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.
[15] ZHANG Baomin,LIU Jingjiang.Classification and characteristics of karst reservoirs in China and related theories[J].Petroleum Exploration and Development,2009,36(1):12-29.
[16] 张恒,蔡忠贤,漆立新,等.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,et al.Hydrogeomorphological condition and its control mechanism on Mid-Lower Ordovician paleo-karst reservoirs,Tazhong uplift[J].Acta Petrolei Sinica,2018,39(9):990-1005.
[17] 杨明德.喀斯特流域水文地貌系统[M].北京:地质出版社,1998.
YANG Mingde.Karst river basin landform system[M].Beijing:Geological Publishing House,1998.
[18] 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 hydor-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.
[19] 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.
[20] 窦之林.碳酸盐岩缝洞型油藏描述与储量计算[J].石油实验地质,2014,36(1):9-15.
DOU Zhilin.Description and reserves calculation of fractured-vuggy carbonate reservoirs[J].Petroleum Geology & Experiment,2014,36(1):9-15.
[21] 韩剑发,苏洲,陈利新,等.塔里木盆地台盆区走滑断裂控储控藏作用及勘探潜力[J].石油学报,2019,40(11):1296-1310.
HAN Jianfa,SU Zhou,CHEN Lixin,et al.Reservoir-controlling and accumulation-controlling of strike-slip faults and exploration potential in the platform of Tarim Basin[J].Acta Petrolei Sinica,2019,40(11):1296-1310.
[22] 王阳洋,陈践发,庞雄奇,等.塔中地区奥陶系油气充注特征及运移方向[J].石油学报,2018,39(1):54-68.
WANG Yangyang,CHEN Jianfa,PANG Xiongqi,et al.Ordovician hydrocarbon charging characteristics and migration direction in Tazhong area[J].Acta Petrolei Sinica,2018,39(1):54-68.
[23] 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.
JIA Chengzao.Tectonic characteristics and petroleum,Tarim Basin,China[M].Beijing:Petroleum Industry Press,1997.
[24] 沈安江,潘文庆,郑兴平,等.塔里木盆地下古生界岩溶型储层类型及特征[J].海相油气地质,2010,15(2):20-29.
SHEN Anjiang,PAN Wenqing,ZHENG Xingping,et al.Types and characteristics of Lower Palaeozoic karst reservoirs in Tarim Basin[J].Marine Origin Petroleum Geology,2010,15(2):20-29.
[25] 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.
[26] 严威,王兴志,张廷山,等.塔河油田加里东中期第Ⅲ幕岩溶作用[J].石油学报,2011,32(3):411-416.
YAN Wei,WANG Xingzhi,ZHANG Tingshan,et al.Investigations of the karst during the Episode III of the mid-Caledonian in the Tahe oilfield[J].Acta Petrolei Sinica,2011,32(3):411-416.
[27] 和虎,冯海霞,蔡忠贤.巴楚隆起先巴扎三维区鹰山组岩溶特征及成因[J].油气地质与采收率,2014,21(5):22-26.
HE Hu,FENG Haixia,CAI Zhongxian.Karst characteristic and origin analysis for Yingshan Formation in Xianbazha 3D area of the Bachu uplift[J].Petroleum Geology and Recovery Efficiency,2014,21(5):22-26.
[28] 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,Tarim Basin[J].Oil & Gas Geology,2016,37(5):674-683.
[29] 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.
[30] TIAN Fei,DI Qingyun,JIN Qiang,et al.Multiscale geological-geophysical characterization of the epigenic origin and deeply buried paleokarst system in Tahe oilfield,Tarim Basin[J].Marine and Petroleum Geology,2019,102:16-32.
[31] 王增银,沈继方,徐瑞春,等.鄂西清江流域岩溶地貌特征及演化[J].地球科学:中国地质大学学报,1995,20(4):439-444.
WANG Zengyin,SHEN Jifang,XU Ruichun,et al.Karst landscapes and their evolution in reaches of the Qingjiang River,western Hubei[J].Earth Science:Journal of China University of Geosciences,1995,20(4):439-444.
[32] 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):377-384.
[33] VEIZER J,ALA D,AZMY K,et al.⁸⁷Sr/⁸⁶Sr,δ¹⁸O and δ¹³C evolution of Phanerozoic seawater[J].Chemical Geology,1999,161(1/3):59-88.
[34] 杨柳,李忠,吕修祥,等.塔中地区鹰山组岩溶储层表征与古地貌识别——基于电成像测井的解析[J].石油学报,2014,35(2):265-275.
YANG Liu,LI Zhong,LV Xiuxiang,et al.Paleotopographic characterization and reconstruction of karst reservoirs in Yingshan Formation,Tazhong area,Tarim Basin:a research based on borehole image log interpretation[J].Acta Petrolei Sinica,2014,35(2):265-275.
[35] 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:地球科学,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 Sciences,2001,44(9):816-823.

塔里木盆地中—下奥陶统岩溶水文地貌结构类型及特征

Types and characteristics of karst hydrogeomorphologic architecture in the Middle-Lower Ordovician,Tarim Basin

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