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天然气地球科学

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塔中北斜坡鹰山组碳酸盐岩沉积微相特征与演化

任凭，林畅松，韩剑发，李浩，刘景彦，王清龙   

  1. 1.中国地质大学(北京)海洋学院，北京100083；2.中国地质大学(北京)能源学院，北京100083；
    3.塔里木油田公司勘探开发研究院，新疆 库尔勒841000
  • 收稿日期:2014-07-09 修回日期:2014-08-28 出版日期:2015-02-10 发布日期:2015-02-10
  • 作者简介:任凭(1990-)，女，新疆库尔勒人，硕士研究生，主要从事含油气盆地分析和碳酸盐岩沉积层序研究.E-mail：pinyren@yeah.net.
  • 基金资助:
    国家重点基础研究发展计划“973”项目“中国西部叠合盆地深部有效碳酸盐岩储层形成机制与分布预测”(编号：2011CB201103);国家油气重大专项“塔中碳酸盐岩凝析气藏高效开发技术”(编号：2011ZX05049)联合资助.
     

Microfacies Characteristics and Depositional Evolution of the Lower Ordovician Yingshan Formation in North Slope of Tazhong Area,Tarim Basin

REN Ping，LIN Chang-son，HAN Jian-fa，LI Hao，LIU Jing-yan，WANG Qing-long   

  1. 1.School of Ocean Sciences,China University of Geosciences,Beijing 100083,China；
    2.School of Energy Resources,China University of Geosciences,Beijing 100083,China；
    3.Research Institute of Exploration and Development,Tarim Oilfield Company,PetroChina,Korla 841000,China
  • Received:2014-07-09 Revised:2014-08-28 Online:2015-02-10 Published:2015-02-10

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摘要：

碳酸盐岩沉积微相不仅揭示了水动力特征及其沉积环境，也是后期储层发育的物质基础，在油气勘探中具有重要意义。通过大量薄片及岩心资料划分出塔中北斜坡鹰山组Mf1—Mf10 10种沉积微相类型，及MA1—MA4 4种沉积微相序列，其在平面上沿塔中一号断裂带呈条带状展布，靠近台地边缘附近多发育高能—中高能滩型微相序列(MA1—MA2)，而台地内部能量相对下降，主要发育中低能潮坪型微相序列(MA3)低能白云质潮坪型微相序列(MA4);从鹰二段至鹰一段沉积时期，由相对低能沉积微相序列(MA3—MA4)向高能沉积微相序列(MA1—MA2)发生转化，鹰一段沉积晚期是滩体形成的主要时期，沉积环境水体能量向上逐渐增强。鹰山组顶部高能沉积微相发育多种孔隙类型，且易于发育构造裂缝并接受岩溶作用改造，是有利储层发育的物质基础。
 

关键词: 塔里木盆地, 鹰山组, 沉积微相, 微相序列

Abstract:

The depositional microfacies of carbonate illustrate the feature of the depositional water energy and environment.Additionally,microfacies are the fundamental of pore space development and facilitate the formation of favorable reservoirs.Ten depositional microfacies (Mf1-Mf10) and four microfacies patterns (MA1-MA4) are recognized in Yingshan Formation,the northern slope of central Tarim Basin,through a large number of thin-sections and cores.The microfacies patterns are distributed horizontally along with the Tazhong No.1 fault zone.High-energy to medium-to-high-energy depositional patterns developed beside the boundary of platform (i.e.MA1 and MA2).However,the microfacies patterns in the inner platform indicate the decrease of water-energy to the central basin.Two microfacies patterns,including medium-to-low-energy tidal flat (MA3) and low-energy-dolomitic tidal flat (MA4),have been suggested in the inner platform.Medium-to-low-energy microfacies patterns transform to medium-to-high-energy microfacies patterns from Yingshan 2nd to Yingshan 1st.During the late stage of Yingshan 1st,which is the main stage for forming carbonate shoals,the depositional water energy gradually increased from the bottom to the top.The high energy microfacies which were on the top of Yingshan Formation,were the primitive material for favorable reservoir,because they formed several types of pores,and developed structural fractures and karstification more easily.

Key words:

中图分类号: 

  • TE122.2+21
［1］Flügel E.Microfacies of Carbonate Rocks:Analysis,Interpretation and Application[M].Germany:Springer,2004:7-52.
［2］Liu Jiaqing,Li Zhong,Huang Juncou,et al.Distinct sediment environments and their influences on carbonate reservoir evolution of Lianglitage Formation in the Tarim Basin,northwest China[J].Science China:Earth Science,2012,42(12):1802-1816.［刘嘉庆,李忠,黄君凑,等.塔里木盆地良里塔格组沉积环境差异及其对碳酸盐储层发育的制约[J].中国科学:地球科学,2012,42(12):1802-1816.］
［3］Zhou Xinyuan,Wang Zhaoming,Yang Haijun,et al.Cases of discovery and exploration of marine fields in China(Part 5):Tazhong Ordovician condensate field in Tarim Basin[J].Marine Origin Petroleum Geology,2006,11(1):45-51.［周新源,王招明,杨海军,等.中国海相油气田勘探实例之五塔中奥陶系大型凝析气田的勘探和发现[J].海相油气地质,2006,11(1):45-51.］
［4］Ji Yungang,Hang Jianfa,Zhang Zhenghong,et al.Formation and distribution of deep high quality reservoirs of Ordovician Yingshan Formation in the northern slop of the Tazhong area in Tarim Basin[J].Acta Geologica Sinica,2012,86(7):1163- 1174.［吉云刚,韩剑发,张正红,等.塔里木盆地塔中北斜坡奥陶系鹰山组深部优质岩溶储层的形成与分布[J].地质学报,2012,86(7):1163-1174.］
［5］Wang Zhaoming,Yang Haijun,Wang Qinghua,et al.Geological Theory and Exploration Technology for Marine Carbonate Giant Condensate Field of Tazhong Uplift in Tarim Basin[M].Beijing:Science Press,2012:18-42.［王招明,杨海军,王清华,等.塔中隆起海相碳酸盐岩特大型凝析气田地质理论与勘探技术[M].北京:科学出版社,2012:18-42.］
［6］Gao Da,Lin Changsong,Yang Haijun,et al.Microfacies of Late Ordovician Lianglitage Formation and their control on favorable reservoir in Tazhong area[J].Journal of China University of Geosciences:Earth Science,2013,38(4):819-831.［高达,林畅松,杨海军,等.塔中地区良里塔格组沉积微相及其对有利储层的控制[J].中国地质大学学报:地球科学,2013,38(4):819-831.］
［7］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):497-500,606.［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］Yang Haijun,Wu Guanghui,Han Jianfa,et al.Characteristics of hydrocarbon enrichment along the Ordovician carbonate platform margin in the central uplift of Tarim Basin[J].Acta Geologica Sinica,2007,28(4):26-30.［杨海军,邬光辉,韩剑发,等.塔里木盆地中央隆起带奥陶系碳酸盐岩台缘带油气富集特征[J].石油学报,2007,28(4):26-30.］
［9］Pan Wenqing,Liu Yongfu,Dickson J,et al.The Geological model of hydrothermal activity in outcrop and the characteristics of carbonate hydrothermal karst of Lower Paleozoic in Tarim Basin[J].Acta Sedimentologica Sinica,2009,27(5):983-994.［潘文庆,刘永福,Dickson J,等.塔里木盆地下古生界碳酸盐岩热液岩溶的特征及地质模型[J].沉积学报,2009,27(5):983-994.］
［10］Yu Hongfeng,Bai Zhongkai,Deng Liping,et al.Determination and geologic significance of Yingshan unconformity of Lower Ordovician in Tazhong area,Tarim Basin[J].XinJiang Petroleum Geology,2011,32(3):231-234.［于红枫,白忠凯,邓力萍,等.塔中下奥陶统鹰山组不整合面的确定及其地质意义[J].新疆石油地质,2011,32(3):231-234.］
［11］Zhao Zongju,Wu Xingning,Pan Wenqing,et al.Sequence lithofacies paleo-geography of Ordovician in Tarim Basin[J].Acta Sedimentologica Sinica,2009,27(5):939-955.［赵宗举,吴兴宁,潘文庆,等.塔里木盆地奥陶纪层序岩相古地理[J].沉积学报,2009,27(5):939-955.］
［12］He Changpo,Wang Zhenyu,Zhang Yunfeng,et al.Study on sedimentary facies types and distribution of the Middle-Lower Ordovician in the north ramp of Tazhong area[J].Xinjiang Oil and Gas,2009,5(2):11-17.［何长坡,王振宇,张云峰,等.塔中北斜坡中下奥陶统鹰山组沉积相类型及分布研究[J].新疆石油天然气,2009,5(2):11-17.］
［13］Wang Hongqiu,Liu Weifang,Zheng Duoming,et al.Types and causes of “none-string beads” fracture-cavity reservoirs in Ordovician carbonate of Tarim Basin[J].Natural Gas Geoscience,2011,22(6):982-988.［王洪求,刘伟方,郑多明,等.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[J].天然气地球科学,2011,22(6):982-988.］
［14］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.［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.］
［15］Tang Hong,Xie Lin,Su Bo,et al.Fracture and vug character of Ordovician carbonate reservoir in Tazhong Oilfield[J].Journal of China University of Petroleum,2013,37(2):7-13.［唐洪,谢琳,苏波,等.塔中奥陶系碳酸盐岩储层缝洞特征[J].中国石油大学学报:自然科学版,2013,37(2):7-13.］
［16］Wang Fuhuan,Wang Zhouming,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):695-702.［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):695-702.］
［17］Hu Xiaolan,Fan Tailiang,Gao Zhiqian,et al.The depositional combination characteristics and distribution of Ordovician carbonate shoals in the Tarim Basin[J].Acta Sedimentologica Sinica,2014,32(3):418-428.［胡晓兰,樊太亮,高志前,等.塔里木盆地奥陶系碳酸盐岩颗粒滩沉积组合及展布特征[J].沉积学报,2014,32(3):418-428.］
［18］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.］
［19］Lin Changsong,Li Hao,Liu Jingyan.Major Unconformity tectonic stratigraphic framework and evolution of the superimposed Tarim Basin[J].Journal of Earth Science,2012,23(4):395-407.
［20］Lin Changsong,Yang Haijun,Liu Jingyan,et al.Distribution and erosion of the Paleozoic tectonic unconformities in the Tarim Basin,northwest China:Significance for the evolution of paleo-uplifts and tectonic geography during deformation[J].Journal of Asian Earth Sciences,2012,46(3):1-19.
［21］Lin Changsong,Yang Haijun,Liu Jingyan,et al.Paleo-structural geomorphology of the Paleozoic central uplift belt and its constraint on the development of depositional facies in the Tarim Basin[J].Science in China:Series D,2009,52(6):823-834.
［22］Lin Changsong,Yang Haijun,Liu Jingyan,et al.Sequence architecture and depositional evolution of the Ordovician carbonate platform margin in the Tarim Basin and its response to tectonics and sea-level change[J].Basin Research,2012,24(5):559-582.
［23］Lin Changsong,Li Sitian,Liu Jingyan,et al.Tectonic framework and paleo-geographic evolution of the Tarim Basin during the Paleozoic major evolutionary stages[J].Acta Petrologica Sinica,2011,27(1):210-218.［林畅松,李思田,刘景彦,等.塔里木盆地古生代重要演化阶段的古构造格局与古地理演化[J].岩石学报,2011,27(1):210-218.］
［24］Lin Changsong,Yang Haijun,Liu Jingyan,et al.Tectonic geomorphology of the Paleozoic central Uplift belt and its constraint on the development of depositional facies in the Tarim Basin[J].China Science:Series D,2009,39(3):306-316.［林畅松,杨海军,刘景彦,等.塔里木盆地古生代中央隆起带古构造地貌及其对沉积相发育分布的制约[J].中国科学：D辑,2009,39(3):306-316.］
［25］Sun Chonghao,Yang Haijun,Pan Wenqing,et al.Fine division of Yingshan Formation of Ordovician in Tazhong area,Tarim Basin[J].Xinjiang Petroleum Geology,2012,33(1):46-48.［孙崇浩,杨海军,潘文庆,等.塔中地区奥陶系鹰山组精细划分[J].新疆石油地质,2012,33(1):46-48.］
[26]Dunham R J.Classification of carbonate rocks according to depositional textures[J].Amer.Assoc.Petrol.Goel.Mem.,1962,(1):108-121.
[27]Wilson J L,Wilson J L.Carbonate Facies in Geologic History[M].New York:Springer-Verlag,1975:25-50.
［27］Pan Wenqing,Hou Guiting,Qi Yingmin,et al.Discussion on the development models of structural fractures in the carbonate rocks[J].Earth Science Frontiers,2013,20(5):188-195.［潘文庆,侯贵廷,齐英敏,等.碳酸盐岩构造裂缝发育模式探讨[J].地学前缘,2013,20(5):188-195.］
 
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