天然气地球科学 ›› 2012, Vol. 23 ›› Issue (4): 748–755.doi: 10.11764/j.issn.1672-1926.2012.04.748

• 天然气地质学 • 上一篇    下一篇

全球显生宇碳酸盐岩储层及油气资源量分布特征

余宽宏,金振奎,潘怡,王哲,杨有星   

  1. 中国石油大学(北京)地球科学学院,北京 昌平 102249
  • 收稿日期:2012-03-06 修回日期:2012-04-12 出版日期:2012-08-10 发布日期:2012-08-10
  • 通讯作者: 余宽宏yukuanhong1983@126.com. E-mail:yukuanhong1983@126.com.
  • 作者简介:余宽宏(1983-),男,四川广元人,博士研究生,主要从事沉积学及储层地质学研究. E-mail:yukuanhong1983@126.com.
  • 基金资助:

    国家重点基础研究发展规划(“973”)项目(编号:2006CB202300)资助.

Phanerozoic Carbonate Reservoir Characteristics   and Petroleum Resource Distribution in the World

YU Kuan-hong,JIN Zhen-kui,PAN Yi,WANG Zhe,YANG You-xing   

  1. Faculty of Geoscience,China University of Petroleum,Beijing 102249,China
  • Received:2012-03-06 Revised:2012-04-12 Online:2012-08-10 Published:2012-08-10

摘要:

通过大量的碳酸盐岩盆地、储层、油气资源量方面的资料收集、总结分析,以显生宇的系为地层单位研究了全球六大油气富集区碳酸盐岩储层及油气资源量的分布特征。中东—欧洲油气区储层主要发育在中生界侏罗系和白垩系;中亚—俄罗斯油气区储层主要分布于上古生界;北美油气区储层主要分布于上古生界;非洲油气区储层主要分布在白垩系及新生界;南美油气区储层主要分布在白垩系;亚太—中国油气区的中国地区储层主要分布在下古生界,而南亚太平洋地区储层则分布于新生界。碳酸盐岩储集岩可以分为石灰岩、白云岩、白垩3种类型,其中以石灰岩及白云岩为主。地质时代越老白云岩储层越多,地质时代越年轻石灰岩储层越多。另外,储层受控于沉积相类型,在高能的滩相以及由泻湖、潮坪等环境形成的白云岩储层最发育;生物建造的储层为最好的油气储集岩体。碳酸盐岩油气资源区域展布受控于盆地的分布。在层系上以白垩系最多,油气资源集中分布在石炭系—新近系,其中石油资源以白垩系最多,天然气以二叠系和白垩系最多,另外在石炭系、侏罗系、古近系均有丰富的油气资源。

关键词: 碳酸盐岩, 油气富集区, 储层特征, 油气资源量, 分布特征

Abstract:

Based on statistics and integrate analysis of data on carbonate basins in the world,we discuss characteristics of carbonate reservoirs,distribution of petroleum  resources in different geologic periods in six regions of enriched oil and gas.High quality reservoirs in Middle East-European region,Central Asia- Russia-North  America,Africa,South America,China-Asia Pacific region,and South Asia-Pacific region are distributed in Jurassic-Cretaceous,upper Paleozoic,Cretaceous-Cenozoic,Cretaceous,lower-Paleozoic,and Cenozoic,respectively.Three types of reservoir lithology are limestone,dolomite and chalk,in which limestone and dolomite   are dominant.The older age the reservoir is,the larger proportion the dolomite is;but the younger age the reservoir is,the larger proportion the limestone  is.Distribution of reservoirs is controlled by deposited facies.The particles beaches,tidal flat and lagoon are profitable to form the dolomite.The deposited  facies for high quality reservoir formation is bioconstructed.Distribution of petroleum resources is controlled by carbonate space.Most of petroleum resource is  distributed from Carboniferous to Tertiary,the oil is dominated in Cretaceous,the gas is Permian and Cretaceous.Additionally,the abundant petroleum resources are  also disturbed in Carboniferous,Jurassic and Paleocene.

Key words: Carbonatite, Petroleum enriched region, Reservoir characteristics, Petroleum resources, Petroleum distribution

中图分类号: 

  • TE122.2

[1]Jiang Huaiyou,Song Xinmin,Wang Yuanji,et al.Current situation and forecast of the world′s carbonate oil and gas exploration and development[J].Offshore Oil,2008,4(6):6-14.[江怀友,宋新民,王元基,等.世界海相碳酸盐岩油气勘探开发现状与展望[J].海洋石油,2008,4(6):6-14.]
[2]Roehl P O,Choquette P W.Introduction[M]//Roehl P O,Choquette P W.Carbonate Petroleum Reservoirs.New York:Springer Verlag,1985:1-15.
[3]Alsharhan A S,Nairn A E M.Sedimentary Basins and Petroleum Geology of the Middle East[M].Amster-dam:Elsevier Science,1997:1-942.
[4]Wilson J L.Limestone and Dolomite Reservoirs[M]//Hobson G D.Developments in Petroleum Geology.London:Applied Science Publishers Ltd,1980:1-51.
[5]Wilson J L.A Review of Carbonate Reservoirs[M].Miall A D.Facts and Principles of World Petroleum Occurrence.Canada:Canadian Society of Petroleum Geologists,Memoir 6,1980:95-117.
[6]Kuznetov V G.Oil and gas in reef reservoirs in the former USSR[J].Petroleum Geoscience,1997,(3):65-71.
[7]Feng Zengzhao,Jin Zhenkui.Lithofacies paleogeography of Permian  in Yunnan,Guizhou and Guangxi[M].Beijing:Geological Publishing House,1994:1-146.[冯增昭,金振奎.滇黔桂地区二叠纪岩相古地理[M].北京:地质出版社,1994:1-146.]
[8]Feng Zengzhao,Peng Yongmin,Jin Zhenkui,et al.Lithofacies Paleogeography of Cambrian-Ordovician in South China[M].Beijing:Geological Publishing  House,2001:1-221.[冯增昭,彭勇民,金振奎,等.中国南方寒武纪-奥陶纪岩相古地理[M].北京:地质出版社,2001:1-221.]
[9]Feng Zengzhao,Yang Yuqing,Jin Zhenkui.Lithofacies Paleogeography of Permian  in South China[M].Dongying:University of Petroleum Press,1997:1-242.[冯增昭,杨玉卿,金振奎.中国南方二叠纪岩相古地理[M].东营:石油大学出版社,1997:1-242.]
[10]Feng Zengzhao,Yang Yuqing,Bao Zhidong,et al.Lithofacies Paleogeography of Carboniferous in South China[M].Beijing:Geological Publishing House,1998:1-119.[冯增昭,杨玉卿,鲍志东,等.中国南方石炭纪岩相古地理[M].北京:地质出版社,1998:1-119.]
[11]Feng Zengzhao,Zhang Jiaqiang,Wang Guoli,et al.Lithofacies Paleogeography of Cambrian:Ordovician in northwest China[M].Dongying:University of Petroleum  Press,2000:1-233.[冯增昭,张家强,王国力,等.中国西北地区寒武纪—奥陶纪岩相古地理[M].东营:石油大学出版社,2000:1-233.]
[12]Jin Zhenkui,Su Kui,Dong Xiaodong,et al.Significance  of oil and gas exploration with the discovery of oil  seepage  in Cambrian strata,northern Yangtz  platform[J].Journal of Palaeogeography,2007:588.[金振奎,苏奎,董晓东,等.扬子地台北缘寒武系油苗的发现及其油气勘探意义[J].古地理学报,2007:588.]
[13]Yu Kuanhong,Jin Zhenkui,Li Peng,et al.Lithofacies paleogeography of Cambrian-Ordovician[J].Eastern Tarim Basin Northwestern Geology,2010,43(4):113-118.[余宽宏,金振奎,李鹏,等.塔东地区寒武—奥陶纪岩相古地理分析[J].西北地质,2010,43(4):113-118.]
[14]Yang Yongjian,Liu Jiaduo,Tian Jingchun,et al.Sequence lithofacies paleogeography of Cambrian in Tarim basin[J].Natural Gas Geoscience,2011,22(3):450-459.[杨永剑,刘家铎,田景春,等.塔里木盆地寒武纪层序岩相古地理特征[J].天然气地球科学,2011,22(3):450-459.]
[15]Su Kui,Jin Zhenkui,Du Hongyu,et al.Lithofacies palaeogeography of the Meishucun Age in the middle and upper Yangtze region[J].Science and Technology Review,2009,27(10):26-31.[苏奎,金振奎,杜宏宇,等.中上扬子地区早寒武世梅树村期岩相古地理[J].科技导报,2009,27(10):26-31.]
[16]Jin Zhenkui,Zou Yuanrong,You Weifeng,et al.Ordovician lithofacies paleogeography of north Bohai Bay basin[J].Acta Sedimentologica Sinica,2002,20(1):13-19.[金振奎,邹元荣,由伟丰,等.渤海湾盆地北部奥陶纪岩相古地理[J].沉积学报,2002,20(1):13-19.]
[17]Dai Jinxing,Zou Caineng,Tao Shizhen,et al.Formation conditions and main controlling factors of large gas fields in China[J].Natural Gas Geoscience,2007,18(4):473-484.[戴金星,邹才能,陶士振,等.中国大气田形成条件和主控因素[J].天然气地球科学,2007,18(4):473-484.]
[18]Dai Jinxing.Enhance the studies on natural gas geology and find more large gas fields in China[J].Natural Gas Geoscience,2003,14(1):3-14.[戴金星.加强天然气地学研究,勘探更多大气田[J].天然气地球科学,2003,14(1):3-14.]
[19]Zhao Wenzhi,Wang Zecheng,Wang Hongjun,et al.Geological characteristic of largemid scale gas fields discoveried recently in China and natural gas prospecting in the Early 21st Century[J].Natural Gas Geoscience,2005,16(6):687-692.[赵文智,汪泽成,王红军,等.近年来我国发现大中型气田的地质特点与21世纪初天然气勘探前景[J].天然气地球科学,2005,16(6):687-692.]
[20]Song Zhenghai.Origin of theory of continental drift[J].Studies in the History of Natural Sciences,1982,1(2):160-166.[宋正海.大陆漂移理论的渊源[J].自然科学史研究,1982,1(2):160-166.]
[21]Chen Shouyuan,Yang Zhijian,Wang Yunshan.On the continental drift towards the west and towards the northern hemisphere[J].Journal of Shandong University of Technology,1996,26(supplement):400-410.[陈寿元,杨志坚,王蕴珊.大陆漂移方向的讨论[J].山东工业大学学报,1996,26(增刊):400-410.]
[22]Qian Weihong.A dynamical model for continental drift and experimental simulated results[J].Journal of Geomechanics,2000,6(1):15-21.[钱维宏.大陆漂移的动力学模式和试验模拟结果[J].地质力学学报,2000,6(1):15-21.]
[23]Steven M T.Plate Tectonics[M].Shanghai:Shanghai Science and Technology Literature Press,2010:1-70.[史蒂芬 M 托梅切克.板块构造[M].上海:上海科学技术文献出版社,2010:1-70.]
[24]Jin Zhenkui,Yu Kuanhong.Characteristics and significance of the burial dissolution of dolomite reservoirs:Taking the lower Palaeozoic in eastern Tarimbasin as an example[J].Petroleum Exploration and Development,2011,38(4):428-434.[金振奎,余宽宏.白云岩储集层埋藏溶蚀作用特征及意义——以塔里木盆地东部下古生界为例[J].石油勘探与开发,2011,38(4):428-434.]
[25]Jin Zhenkui,Feng Zengzhao.Origin of Dolostones of the lower Permian in east Yunnan-west Sichuan:Dolomitization through leaching of basalts[J].Acta  Sedimentologica Sinica,1999,17(3):383-389.[金振奎,冯增昭.滇东—川西下二叠统白云岩的形成机理——玄武岩淋滤白云化[J].沉积学报,1999,17(3):383-389.]
[26]Jin Zhenkui,Feng Zengzhao.Significance  and types of lower-Paleozoic dolomite in eastern north China platform[J].Acta Sedimentologica Sinica,1993,11 (2):11-19.[金振奎,冯增昭.华北地台东部下古生界白云岩的类型及储集性能[J].沉积学报,1993,11(2):11-19.]
[27]Yu Kuanhong,Jin Zhenkui,Zhou Yong,et al.Dolomitization in deepwater environment of Cambrian in penecontemporaneous diagenetic stage,eastern Tarim basin[J].Acta Sedimentologica Sinica,2011,29(6):56-63.[余宽宏,金振奎,周勇,等.塔里木盆地东部地区寒武纪海盆局限期深水准同生白云化作用研究[J].沉积学报,2011,29(6):56-63.]
 [28]Gerhard L C,Anderson S B,Lefever J A,et al.Geological development,origin,and energy mineral resources of Williston basin,north Dakota[J].AAPG  Bulletin,1982,66:989-1020.
[29]Fan Jiasong,Wu Yasheng.Restudy of the Permian reefs in eastern Sichuan,China[J].Oil and Gas Geology,2002,23(1):12-18.
[30]Alsharhan A S,St Kendall C G C.Precambrian to Jurassic rocks of Arabian gulf and adjacent areas:Their facies,depositional setting,and hydrocarbon habitat[J].AAPG Bulletin,1986,70:977-1002.
[31]Roehl P O,Choquette P W.Carbonate Petroleum Reservoirs[M].Berlin,Heidelberg,New York:Springer Verlag,1985:1-622.
[32]Reeckmann A,Friedman G M.Exploration for Carbonate Petroleum Reservoirs[M].New York:John Wiley & Sons,1982:1-213.
[33]Fan Jiasong.Characteristics of carbonate reservoirs for oil and gas fields in the world and essential controlling factors for their formation[J].Earth  Science Frontiers,2005,13(3):23-29.[范嘉松.世界碳酸盐岩油气田的储层特征及其成藏的主要控制因素[J].地学前缘,2005,13(3):23-29.]
[34]Jiao Weiwei,Li Jianjiao,Tian Lei,et al.Geological conditions of marine carbonate high-quality reservoir in China[J].Geological Science and Technology  Information,2009,28(6):64-70.[焦伟伟,李建交,田磊,等.中国海相碳酸盐岩优质储层形成的地质条件[J].地质科技情报,2009,28(6):64-70.]
[35]
[JP3]Luo Ping,Zhang Jing,Liu Wei,et al.Characteristics of marine carbonate hydrocarbon reservoirs in China[J].Earth Science Frontiers,2008,15(1):36-50.[罗平,张静,刘伟,等.中国海相碳酸盐岩油气储层基本特征[J].地学前缘,2008,15(1):36-50.]
[36]Wan Jing,Sun Yupeng.Analysis of main controlling factors of formation evolution in grain-beach carbonate reservoir[J].Oil-Gas Blocked Deposit,2009,16(4):60-62.[万晶,孙玉朋.颗粒滩相碳酸盐岩储层发育演化的主控因素[J].断块油气藏,2009,16(4):60-62.]
[37]Zhang Xuefeng,Liu Bo,Cai Zhongxian,et al.Dolomitization and carbonate reservoir formation[J].Geological Science and Technology Information,2010,29(3):79-85.[张学丰,刘波,蔡忠贤,等.白云岩化作用与碳酸盐岩储层物性[J].地质科技情报,2010,29(3):79-85.]
[38]Zhao Zongju,Fan Guozhang,Wu Xingning,et al.Reservoir types,exploration domains and exploration strategy of marine carbonates in China[J].Marine Origin  Petroleum Geology,2007,12(1):1-11.[赵宗举,范国章,吴兴宁,等.中国海相碳酸盐岩的储层类型、勘探领域及勘探战略[J].海相油气地质,2007,12(1):1-11.]
[39]Chen Jinyong,Li Zhenpeng.Major controlling factors of carbonate rock reservoirs[J].Marine Geology Letters,2010,26(4):19-25.[陈金勇,李振鹏.碳酸盐岩储层的主要影响因素[J].海洋地质动态,2010,26(4):19-25.]
[40]Bai Guoping.Distribution patterns of giant carbonate fields in the world[J].Journal of Palaeogeography,2006,8(2):241-250.[白国平.世界碳酸盐岩大油气田分布特征[J].古地理学报,2006,8(2):241-250.]
[41]Bai Guoping,Zheng Lei.Distribution patterns of giant gas fields in the world[J].Natural Gas Geoscience,2007,18(2):161-167.[白国平,郑磊.世界大气田分布特征[J].天然气地球科学,2007,18(2):161-167.]

[1] 王清龙,林畅松,李浩,韩剑发,孙彦达,何海全. 塔里木盆地西北缘中下奥陶统碳酸盐岩沉积微相特征及演化[J]. 天然气地球科学, 2018, 29(9): 1274-1288.
[2] 吕正祥,王先东,吴家洋,卿元华. 渤海海域中部古近系湖相碳酸盐岩储层成岩演化特征[J]. 天然气地球科学, 2018, 29(7): 921-931.
[3] 王珊,曹颖辉,杜德道,王石,李洪辉,董洪奎,严威,白莹. 塔里木盆地柯坪—巴楚地区肖尔布拉克组储层特征与主控因素[J]. 天然气地球科学, 2018, 29(6): 784-795.
[4] 王国龙,杜社宽. 准噶尔盆地北三台凸起二叠系梧桐沟组一段碎屑岩储层特征及控制因素[J]. 天然气地球科学, 2018, 29(5): 675-681.
[5] 史文洋,姚约东,程时清,石志良,高敏. 裂缝性低渗透碳酸盐岩储层酸压改造油井动态压力特征[J]. 天然气地球科学, 2018, 29(4): 586-596.
[6] 张永庶,伍坤宇,姜营海,王鹏,蔡智洪,高发润,谭武林,高树芳,鲜本忠. 柴达木盆地英西深层碳酸盐岩油气藏地质特征[J]. 天然气地球科学, 2018, 29(3): 358-369.
[7] 孟凡坤,雷群,徐伟,何东博,闫海军,邓惠. 应力敏感碳酸盐岩复合气藏生产动态特征分析[J]. 天然气地球科学, 2018, 29(3): 429-436.
[8] 魏新善,魏柳斌,任军峰,蔡郑红,周黎霞. 鄂尔多斯盆地下古生界风化壳气藏差异性[J]. 天然气地球科学, 2018, 29(2): 178-188.
[9] 李国欣, 易士威, 林世国, 高阳, 李明鹏, 李德江, 王昌勇. 塔里木盆地库车坳陷东部地区下侏罗统储层特征及其主控因素[J]. 天然气地球科学, 2018, 29(10): 1506-1517.
[10] 胡安平,沈安江,潘立银,王永生,李娴静,韦东晓. 二元同位素在碳酸盐岩储层研究中的作用[J]. 天然气地球科学, 2018, 29(1): 17-27.
[11] 王媛,林畅松,李浩,孙彦达,何海全,王清龙,姬牧野,张曼莉. 高频层序地层格架中碳酸盐岩成岩作用研究——以哈萨克斯坦Marsel探区下石炭统谢尔普霍夫阶为例[J]. 天然气地球科学, 2018, 29(1): 28-41.
[12] 赵志平,官大勇,韦阿娟,刘朋波,付立. 渤海海域新生界地层水化学特征及主控因素[J]. 天然气地球科学, 2017, 28(9): 1396-1405.
[13] 贾成业,贾爱林,韩品龙,王建君,袁贺,乔辉. 四川盆地志留系龙马溪组优质页岩储层特征与开发评价[J]. 天然气地球科学, 2017, 28(9): 1406-1415.
[14] 张宫,冯庆付,武宏亮,王克文,冯周. 基于核磁T2谱对数均值差异的碳酸盐岩气水识别[J]. 天然气地球科学, 2017, 28(8): 1243-1249.
[15] 姜黎明,余春昊,齐宝权,朱涵斌,王勇军. 孔洞型碳酸盐岩储层饱和度建模新方法及应用[J]. 天然气地球科学, 2017, 28(8): 1250-1256.
Viewed
Full text


Abstract

Cited

  Shared   
  Discussed   
No Suggested Reading articles found!