天然气地球科学

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塔里木盆地塔河10区奥陶系断裂特征及对岩溶储层的控制作用

韩长城1,林承焰1,任丽华1,鲁新便2,魏婷3,张宪国1   

  1. 1.中国石油大学(华东)地球科学与技术学院,山东 青岛 266580;
    2.中国石化西北油田分公司,新疆 乌鲁木齐 830011;
    3.中国石油新疆油田分公司石西采油厂,新疆 克拉玛依  834000
  • 收稿日期:2015-07-10 修回日期:2015-09-05 出版日期:2016-05-10 发布日期:2016-05-10
  • 作者简介:韩长城(1984-),男,新疆阿勒泰人,博士研究生,主要从事碳酸盐岩油藏精细描述研究. E-mail:517892849@qq.com.
  • 基金资助:
    国家重大科技专项“复杂油气藏精细表征及剩余油分析预测”(编号:2011ZX05009-003);国家自然科学基金项目(编号:41202092);中国石油大学(华东)研究生创新工程项目(编号:YCXJ2016003)联合资助.

Characteristics of Ordovician fault in the Block 10 of Tahe Oilfield, Tarim Basin and its controlling effect on karst reservoirs

Han Chang-cheng1,Lin Cheng-yan1,Ren Li-hua1,Lu Xin-bian2,Wei Ting3,Zhang Xian-guo1   

  1. 1.School of Geosciences,China University of Petroleum,Qingdao 266580,China;
    2.Northwest Oilfield Company,SINOPEC,Urumqi 830011,China;
    3.Shixi Oil Production Plant,Xinjiang Oilfield Company,PetroChina,Karamay 834000,China
  • Received:2015-07-10 Revised:2015-09-05 Online:2016-05-10 Published:2016-05-10

摘要: 随着塔里木盆地奥陶系碳酸盐岩油藏勘探与开发的进展,断裂对碳酸盐岩岩溶储层的控制作用越来越受到关注。通过岩心、薄片、钻井和测井等资料,分析溶蚀洞穴型、溶蚀孔缝型和裂缝型3类储集体特征;从构造演化特征方面对断裂进行分期,根据断裂期次、规模及对岩溶储层的控制作用将断裂分为Ⅱ级、Ⅲ1级和Ⅲ2级,并系统探讨了断裂对岩溶储层的发育和油气成藏的控制作用。综合分析结果表明,塔河油田10区奥陶系主要发育加里东中晚期、海西早期和海西晚期3期断裂,其中海西期断裂对岩溶储层的形成和发育起着决定作用,Ⅱ级和Ⅲ1级断裂对岩溶储层发育和油气成藏控制作用最为重要。断裂不仅促使表层岩溶作用发生和岩溶储层形成,控制古地貌的形态、古水系分布和热液岩溶作用的发生,促进深部岩溶作用发生和裂缝的发育,同时断裂对油气运移和聚集也起着重要的控制作用。该认识对碳酸盐岩油气进一步勘探开发具有重要的参考作用。

关键词: 深部岩溶储层, 断裂分期, 断裂分级, 碳酸盐岩储集体, 岩溶作用

Abstract: As with the development of exploring and developing of Ordovician carbonate reservoirs in Tarim Basin,the controlling effect of fault on carbonate reservoirs has drawn more and more attention.On the basis of cores,thin sections,drilling and well-logginganalyses,the reservoir is classified into three types,dissolution vug,dissolution pore-fracture and fractures.According to the structural evolution characteristics,taking fault times,scale and the controlling effect of karst reservoirs into consideration,the faults are classified into three grades including grade Ⅱ,grade Ⅲ-1 and grade Ⅲ-2.Faults’ controlling effect on the development of karst reservoirs and oil and gas entrapment were systematicallysummarized.Based on the comprehensive analysis,Ordovician in the Block 10 of Tahe Oilfield mainly developed three periods of faults,respectively in Late Caledonian,Early Hercynian and Late Hercynian.The Hercynian fracture plays decisive role in the formation and development of karst reservoirs,and grade Ⅱ and grade Ⅲ-1 turn out to be the most important for the development of karst reservoirs and oil and gas entrapment.Faults not only promote development of shallow karst and the formation of fractures,but also control the ancient geomorphology,the distribution of ancient water system and hydrothermal karstification.At the same time,the faults also play an important role in controlling the migration and accumulation of oil and gas.The understanding provides significant guidance of further exploration and development of carbonate oil and gas reservoir.

Key words: Deep karst reservoirs, Fault stage, Fault grading, Carbonate reservoirs, Karstification

中图分类号: 

  • TE122.2

[1]Zhang Xuefeng,Li Ming,Chen Zhiyong,et al.Characteristics and karstification of the Ordovician carbonate reservoir,Halahatang area,northern Tarim Basin[J].Acta Petrologica Sinica,2012,28(3):815-826.[张学丰,李明,陈志勇,等.塔北哈拉哈塘奥陶系碳酸盐岩岩溶储层发育特征及主要岩溶期次[J].岩石学报,2012,28(3):815-826.]
[2]Wan Yun,Liu Cunge,Liu Hong,et al.Identification signs of multiphase karstification of Ordovician reservoir in Tahe Oilfield[J].Journal of China University of Petroleum:Edition of Natural Science,2009,33(5):6-11.[万云,刘存革,刘洪,等.塔河油田奥陶系多期岩溶作用的识别标志[J].中国石油大学学报:自然科学版,2009,33(5):6-11.]
[3]Ren Ping,Lin Changsong,Han Jianfa,et al.Microfacies characteristics and depositional evolution of the Lower Ordovician Yingshan Formation in north slope of Tazhong area,Tarim Basin[J].Natural Gas Geoscience,2015,26(2):241-251.[任凭,林畅松,韩剑发,等.塔中北斜坡鹰山组碳酸盐岩沉积微相特征与演化[J].天然气地球科学,2015,26(2):241-251.]
[4]Ding Yong,Peng Shoutao,Li Huijun.Features and main controlling factors of carbonate reservoirs in Tahe Oilfield and northern Tarim Basin[J].Petroleum Geology & Experiment,2011,33(5):488-494.[丁勇,彭守涛,李会军.塔河油田及塔北碳酸盐岩油藏特征与成藏主控因素[J].石油实验地质,2011,33(5):488-494.]
[5]Liu Zhongbao,Wu Shiqiang,Liu Shilin,et al.Types and main controlling factors of Ordovician reservoirs in Yubei area,Tarim Basin[J].Acta Petrolei Sinica,2013,34(4):638-646.[刘忠宝,吴仕强,刘士林,等.塔里木盆地玉北地区奥陶系储层类型及主控因素[J].石油学报,2013,34(4):638-646.]
[6]Wu Guanghui,Guo Qunying,Zhu Haiyan,et al.Characteristics of Ordovician fracture-vuggy carbonate reservoir in Mazatage structure belt Tarim Basin[J].Natural Gas Geoscience,2012,23(3):443-449.[邬光辉,郭群英,朱海燕,等.塔里木盆地玛扎塔格构造带奥陶系岩溶缝洞体发育特征[J].天然气地球科学,2012,23(3):443-449.]
[7]Shi Shuyuan,Hu Suyun,Liu Wei,et al.Ordovician paleo-karst cave system and it’s controlling factor in Xekar,Tarim Basin[J].Natural Gas Geoscience,2014,25(2):167-177.[石书缘,胡素云,刘伟,等.塔里木盆地西克尔地区奥陶系溶洞系统特征及控制因素[J].天然气地球科学,2014,25(2):167-177.]
[8]Wu Fangfang,Zhu Guangyou,Zhang Shuichang,et al.Ordovician Hydrocarbon accumulation and main controlling factors in the western margin of Tazhong No.1 Slope-break Zone,Tarim Basin[J].Geological Review,2012,56(3):339-348.[武芳芳,朱光有,张水昌,等.塔里木盆地塔中Ⅰ号断裂带西缘奥陶系油气成藏与主控因素研究[J].地质论评,2012,56(3):339-348.]
[9]Zhang Qingyu,Liang Bin,Cao Jianwen,et al.Palaeokarst modeling for outcrops in Tabei,Tarim Basin[J].Marine Geology Frontiers,2013,29(12):32-36.[张庆玉,梁彬,曹建文,等.塔里木盆地塔北露头区的古岩溶发育模式[J].海洋地质前沿,2013,29(12):32-36.]
[10]Wu Guanghui,Yang Haijun,Qu Tailai,et al.The fault system characteristics and its controlling roles on marine carbonate hydrocarbon in the Central Uplift,Tarim Basin[J].Acta Petrologica Sinica,2012,28(3):793-805.[邬光辉,杨海军,屈泰来,等.塔里木盆地塔中隆起断裂系统特征及其对海相碳酸盐岩油气的控制作用[J].岩石学报,2012,28(3):793-805.]
[11]]Miao Jijun,Jia Chengzao,Zou Caineng,et al.Characteristics and exploration fields of paleo-karst reservoirs at the top of early Ordovician in Central Tarim Uplift[J].Natural Gas Geoscience,2007,18(4):497-500.[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.]
[12]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):317-330.[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):317-330.]
[13]Zhao Xuefeng,Zhu Guangyou,Liu Qinfu,et al.Main control factors if pore development in deep marine carbonate reservoirs[J].Natural Gas Geoscience,2007,18(4):514-521.[赵雪凤,朱光有,刘钦甫,等,深部海相碳酸盐岩储层孔隙发育的主控因素研究[J].天然气地球科学,2007,18(4):514-521.]
[14]Billi A,Valle A,Brilli M,et al.Fracture-controlled fluid circulation and dissolutional weathering in sinkhole-prone carbonate rocks from central Italy[J].Journal of Structural Geology,2007,29(9):385-395.
[15]Zheng Herong,Liu Chunyan,Wu Maobing,et al.Burial dissolution of Ordovician granule limestone in Tarim Basin[J].Acta Petrolei Sinica,2009,30(1):9-15.[郑和荣,刘春燕,吴茂炳,等.塔里木盆地奥陶系颗粒石灰岩埋藏溶蚀作用[J].石油学报,2009,30(1):9-15.]
[16]Li Meng,Tang Liangjie,Qi Lixin,et al.Differential tectonic evolution and its controlling on hydrocarbon accumulation in the south slope of Tabei Uplift[J].Natural Gas Geoscience,2015,26(2):218-228.[李萌,汤良杰,漆立新,等.塔北隆起南坡差异构造演化及其对油气成藏的控制[J].天然气地球科学,2015,26(2):218-228.]
[17]Wu Guanghui,Li Jianjun,Yang Shuanrong,et al.Fractal characteristics of fissures and fractures of Ordovician carbonate rocks in the central Tarim area[J].Chinese Journal of Geology,2002,37(supplement):51-56.[邬光辉,李建军,杨栓荣,等.塔里木盆地中部地区奥陶纪碳酸盐岩裂缝与断裂的分形特征[J].地质科学,2002,37(增刊):51-56.]
[18]An Haiting,Li Haiyin,Wang Jianzhong,et al.Tectonic evolution and its controlling on oil and gas accumulation in the northern Tarim Basin[J].Geotectonica et Metallogenia,2009,33(1):142-147.[安海亭,李海银,王建忠,等.塔北地区构造和演化特征及其对油气成藏的控制[J].大地构造与成矿学,2009,33(1):142-147.]
[19]Cui Zehong,Wang Zhixin,Tang Liangjie.Characteristics of overlapped faults in the north of the Tabei Uplift and analysis of their genetic setting[J].Geology in China,2005,32(3):378-385.[崔泽宏,王志欣,汤良杰.塔北隆起北部叠加断裂构造特征与成因背景分析[J].中国地质,2005,32(3):378-385.]
[20]Wu Xingwei,Yuan Gang,Chen Guangxin,et al.Controlling effects of fault over Ordovician Palaeokarst in Tahe region[J].Fault-Block Oil & Gas Field,2005,12(3):7-9.[邬兴威,苑刚,陈光新,等.塔河地区断裂对奥陶系古岩溶的控制作用[J].断块油气田,2005,12(3):7-9.]
[21]Yu Shun,Liu Guangdi,Sun Mingliang,et al.Controlling effects of fault system on marine Ordovician carbonate hydrocarbon enrichment in eastern Lungu area,Tabei Uplift[J].Geological Science and Technology Information,2014,33(1):121-127.[喻顺,柳广弟,孙明亮,等.断裂系统对碳酸盐岩油气聚集的控制作用——以塔北隆起轮古东油气田为例[J].地质科技情报,2014,33(1):121-127.]
[22]Liu Xiaoping,Sun Dongsheng,Wu Xinsong.Ordovician palaeokarst landform and its control on reservoirs west Lungu region,the Tarim Basin[J].Petroleum Geology & Experiment,2007,29(3):265-268.[刘小平,孙冬胜,吴欣松.古岩溶地貌及其对岩溶储层的控制——以塔里木盆地轮古西地区奥陶系为例[J].石油实验地质,2007,29(3):265-268.]
[23]Qiao Zhanfeng,Shen Anjiang,Zou Weihong,et al.A fault-controlled Non-exposed Meteoric karstification:A case study of Ordovician carbonate reservoir at structure YM2 in northern Tarim Basin,northwestern China[J].Acta Geologica Sinica,2011,85(12):2070-2083.[乔占峰,沈安江,邹伟宏,等.断裂控制的非暴露型大气水岩溶作用模式——以塔北英买2构造奥陶系碳酸盐岩储层为例[J].地质学报,2011,85(12):2070-2083.]
[24]Li Peng,Ren Jianye,Yang Huaizhong,et al.Hydrothermal activities in the fault system and their effects on carbonate rocks in the Bachu area[J].Geotectoncia et Metallogenia,2011,35(3):378-385.[李朋,任建业,阳怀忠,等.巴楚地区断裂带内热液流体活动及对碳酸盐岩改造的特征分析[J].大地构造与成矿学,2011,35(3):378-385.]
[25]Ding Yong,Peng Shoutao,Li Huijun.Features and main controlling factors of carbonate reservoirs in Tahe Oilfield and northern Tarim Basin[J].Petroleum Geology & Experiment,2011,33(5):488-494.[丁勇,彭守涛,李会军.塔河油田及塔北碳酸盐岩油藏特征与成藏主控因素[J].石油实验地质,2011,33(5):488-494.]

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[3] 邬光辉, 郭群英, 朱海燕, 马锋, 冯晓军, 李洪辉. 塔里木盆地玛扎塔格构造带奥陶系岩溶缝洞体发育特征[J]. 天然气地球科学, 2012, 23(3): 443-449.
[4] 苗继军, 贾承造, 邹才能, 邓述友, 苟柱明, 宋玉斌, 侯向辉. 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.
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