岩性油气藏 ›› 2022, Vol. 34 ›› Issue (5): 1–25.doi: 10.12108/yxyqc.20220501

• 地质勘探 • 上一篇    下一篇

川东北二叠系长兴组碳酸盐岩云化成储机制

何文渊1,2, 云建兵3, 钟建华4,5   

  1. 1. 中国石油大庆油田有限责任公司, 黑龙江 大庆 163002;
    2. 黑龙江省陆相页岩油重点实验室, 黑龙江大庆 163712;
    3. 中国石油大庆油田有限责任公司 勘探事业部, 黑龙江 大庆 163712;
    4. 东北大学秦皇岛分校 海洋油气勘探国家研究分中心, 河北 秦皇岛 066004;
    5. 中国石油大学(华东), 山东 青岛 266528)
  • 收稿日期:2022-04-29 修回日期:2022-05-13 出版日期:2022-09-01 发布日期:2022-09-06
  • 通讯作者: 钟建华(1957-),男,博士,教授,博士生导师,主要从事沉积学与构造地质学方面的研究工作。Email:957576033@qq.com。 E-mail:957576033@qq.com。
  • 作者简介:何文渊(1974-),男,博士,教授级高级工程师,主要从事石油地质和油气勘探开发方面的研究工作。地址:(163712)黑龙江大庆市让胡路区。Email:hewy@cnpc.com.cn
  • 基金资助:
    国家重点基础研究发展计划“973”计划“碳酸盐岩缝洞型油藏缝洞单元储集空间成因和控制因素”(编号:2011CB101001)与国家科技重大专项“溶洞型储集体内部结构模式及分布规律研究”(编号:2011ZX05014-002-002)联合资助

Reservoir-forming mechanism of carbonate dolomitization of Permian Changxing Formation in northeastern Sichuan Basin

HE Wenyuan1,2, YUN Jianbing3, ZHONG Jianhua4,5   

  1. 1. PetroChina Daqing Oilfield Company, Daqing 163002, Heilongjiang, China;
    2. Heilongjiang Provincial Key Laboratory of Continental Shale Oil, Daqing 163712, Heilongjiang, China;
    3. Exploration Department, PetroChina Daqing Oilfield Company, Daqing 163712, Heilongjiang, China;
    4. National Research Branch Center for Offshore Oil and Gas Exploration, Northeastern University at Qinhuangdao, Qinhuangdao 066004, Hebei, China;
    5. China University of Petroleum(East China), Qingdao 266528, Shandong, China
  • Received:2022-04-29 Revised:2022-05-13 Online:2022-09-01 Published:2022-09-06

摘要: 四川盆地是我国重要的含油气盆地,其中川东北二叠系长兴组碳酸盐岩是重要的产气地层。近年来发现的普光、龙岗、元坝等天然气田是重要的西气东输基地,对国家油气战略安全具有重要贡献作用。通过野外露头样品及钻井岩心分析,对川东北二叠系长兴组碳酸盐岩云化成储机制及主控因素进行了系统梳理。研究结果表明:①川东北二叠系长兴组气藏主要是一种白云岩气藏,生物礁灰岩储集能力较差与沥青充填有关,为气源层。野外露头考察发现礁盖白云岩具有更优的储集性能,但普光长兴组顶部的白云岩为一种非礁盖白云岩,揭示了长兴顶部的纯白云岩本身就是含气储层,与生物礁关系不大。②川东北长兴组白云岩储层的储集空间包括溶洞、晶间孔、晶内溶孔和晶间缝,为成岩过程中彻底云化而成。③川东北长兴组白云岩化存在5种成因机理:暴露淡水淋滤与蒸发泵流作用、渗透回流或盐水回流台地交代作用、埋藏成岩白云岩化、热液白云岩化、风化交代白云岩化,以前两种为主。表生和早期成岩的白云岩受沉积微相控制,不同区域具有不同的成因模式。川东北生物礁常常发生白云岩化作用,尤其是生物礁顶部,白云岩化后储集性能得到较大改善。④研究区长兴组中上部白云岩气藏的发现具有重要的理论意义和工业价值,尤其是长兴组顶部的白云岩自身具有良好的天然气储集能力,在封盖条件较好的广大区域均可形成工业气藏,川东北开江—梁平海槽台缘外(包括平昌海槽)长兴组也存在发育工业大气田的潜力。

关键词: 蒸发泵, 渗透回流, 白云岩化, 生物礁, 缝洞型储层, 天然气, 长兴组, 二叠系, 川东北

Abstract: Sichuan Basin is an important petroliferous basin in China,and carbonate rocks of Permian Changxing Formation in northeastern Sichuan Basin are important gas producing strata. The natural gas fields discovered in recent years such as Puguang,Longgang and Yuanba are important bases for West-to-East Gas Transmission,and play an important role in the national oil and gas strategic security. Based on the analysis of field outcrop samples and drilling cores,reservoir-forming mechanism of carbonate dolomitization and main controlling factors of Permian Changxing Formation in northeastern Sichuan Basin were analyzed. The results show that:(1)The gas reservoir of Permian Changxing Formation in northeastern Sichuan Basin is mainly dolomitic gas reservoir,and the poor reservoir capacity of reef limestone is related to asphalt filling,which is a gas source layer. The reef cap dolomite has more developed reservoir space according to field outcrop investigation. The dolomite at the top of Changxing Formation in Puguang gas field is a kind of non-reef-cap dolomite,which reveals that the pure dolomite at the top of Changxing Formation is a gas-bearing reservoir and has little relationship with biogenic reef. (2)The reservoir space of dolomitic reservoirs of Changxing Formation in northeastern Sichuan Basin includes karst caves,intercrystalline pores,intracrystalline dissolved pores and intracrystalline fracture,which are completely formed by dolomitization in the process of diagenesis.(3)There are five genetic mechanisms for dolomitization of Changxing Formation in northeastern Sichuan Basin:exposed fresh water leaching and evaporation pumping,seepage reflux or saline reflux platform metasomatism,buried diagenetic dolomitization,hydrothermal dolomitization and weathering metasomatic dolomitization,with the former two being dominant. Supergene and early diagenetic dolomites are controlled by sedimentary microfacies,and there are different genetic models in different regions. Dolomitization often occurs in reefs in northeastern Sichuan Basin,especially at the top of reefs. The reservoir properties have been greatly improved after dolomitization.(4)The discovery of dolomitic gas reservoirs at the middle and upper part of Changxing Formation in the study area is of great theoretical significance and industrial value. The dolomite at the top of Changxing Formation has good natural gas storage capacity, and industrial gas reservoirs can be formed as long as the corresponding conditions are available. Changxing Formation outside the platform margin of Kaijiang-Liangping trough(including Pingchang trough)has the potential of large industrial gas fields.

Key words: evaporation pumping, seepage reflux, dolomitization, biogenic reef, fractured-vuggy reservoir, natural gas, Changxing Formation, Permian, northeastern Sichuan Basin

中图分类号: 

  • TE121.3
[1] 王一刚,张静,杨雨,等.四川盆地东部上二叠统长兴组生物礁气藏形成机理[J].海相油气地质,2000,5(1/2):145-152. WANG Yigang,ZHANG Jing,YANG Yu,et al. Formation mechanism of reef gas reservoirs in the Upper Permian Changxing Formation,eastern Sichuan Basin[J]. Marine Petroleum Geology,2000,5(1/2):145-152.
[2] 王一刚,文应初,张帆,等.川东地区上二叠统长兴组生物礁分布规律[J].天然气工业,1998,18(6):10-15. WANG Yigang,WEN Yingchu,ZHANG Fan,et al. Distribu- tion of organic reefs in the Upper Permian Changxing Forma- tion,eastern Sichuan[J]. Natural Gas Industry,1998,18(6):10-15.
[3] 徐强,刘宝珺,何汉漪,等.四川晚二叠世生物礁层序地层岩相古地理编图[J].石油学报,2004,25(2):47-50. XU Qiang,LIU Baojun,HE Hanyi,et al. Sequence stratigraphy lithofacies and paleogeography mapping for the Late Permian reef in Sichuan Basin[J]. Acta Petrolei Sinica,2004,25(2):47- 50.
[4] 牟传龙,马永生,王瑞华,等.川东北地区上二叠统盘龙洞生物礁成岩作用研究[J]. 沉积与特提斯地质,2005,25(1/2):198-202. MU Chuanlong,MA Yongsheng,WANG Ruihua,et al. Diagen- esis of the Upper Permian Panlongdong organic reefs in north- eastern Sichuan[J]. Sedimentary Geology and Tethyan Geology, 2005,25(1/2):198-202.
[5] 王瑞华,牟传龙,谭钦银,等.达县-宣汉地区长兴组礁滩白云岩成岩作用与成岩环境研究[J].沉积与特提斯地质,2006, 26(1):30-36. WANG Ruihua,MU Chuanlong,TAN Qinyin,et al. Diagenesis processes and environments of the reef shoal dolostones from the Changxing Formation in the Daxian-Xuanhan region,north- eastern Sichuan[J]. Sedimentary Geology and Tethyan Geology, 2006,26(1):30-36.
[6] 洪海涛,王一刚,杨天泉,等.川北地区长兴组沉积相和生物礁气藏分布规律[J].天然气工业,2008,28(1):38-41. HONG Haitao,WANG Yigang,YANG Tianquan,et al. Sedi- mentary facies of Changxing Formation and distribution of or- ganic reef gas reservoirs in northern Sichuan Basin[J]. Natural Gas Industry,2008,28(1):38-41.
[7] 夏明军,曾大乾,邓瑞健,等.普光气田长兴组台地边缘礁、滩沉积相及储层特征[J]. 天然气地球科学,2009,20(4):549- 562. XIA Mingjun,ZENG Daqian,DENG Ruijian,et al. Reef and shallow facies and reservoir characteristics in Changxing Formation platform margin,Puguang gas field[J]. Natural Gas Geo- science,2009,20(4):549-562.
[8] 文华国,郑荣才,党录瑞,等.四川盆地东部五百梯地区长兴组礁、滩相储层特征[J].岩性油气藏,2010,22(2):24-31. WEN Huaguo,ZHENG Rongcai,DANG Lurui,et al. Charac- teristics of reef and shoal facies reservoir of Upper Permian Changxing Formation in Wubaiti area,eastern Sichuan Basin[J]. Lithologic Reservoirs,2010,22(2):24-31.
[9] 曾大乾,彭鑫岭,刘志远,等. 普光气田礁滩相储层表征方法[J].天然气工业,2011,31(3):9-13. ZENG Daqian,PENG Xinling,LIU Zhiyuan,et al. Characterization methods of reef beach facies reservoirs in the Puguang gas field[J]. Natural Gas Industry,2011,31(3):9-13.
[10] LI Hongtao,LONG Shengxiang,YOU Yuchun,et al. Sequence and sedimentary features of the Changxing Fm organic reefs and their control on reservoir development in the Yuanba gas field,Sichuan Basin[J]. Natural Gas Industry B,2015,2(6):506-514.
[11] 钟建华,温志峰,李勇,等. 生物礁的研究现状与发展趋势[J]. 地质论评,2005,51(3):288-300. ZHONG Jianhua,WEN Zhifeng,LI Yong,et al. Organic reefs study:Concept,classification,characteristics,history and development[J]. Geological Review,2005,51(3):288-300.
[12] RIDING R. Cyanophyte calcification and changes in ocean chemistry[J]. Nature,1982,299:814-815.
[13] RIDING R. Structure and composition of organic reefs and car- bonate mud mounds:Concepts and categories[J]. Earth-Science Reviews,2002,58(1/2):163-231.
[14] 郑荣才,胡忠贵,冯青平,等.川东北地区长兴组白云岩储层的成因研究[J].矿物岩石,2007,27(4):78-84. ZHENG Rongcai,HU Zhonggui,FENG Qingping,et al. Gene- sis of dolomite reservoir of the Changxing Formation of Upper Permian,northeast Sichuan Basin[J]. Journal of Mineralogy and Petrology,2007,27(4):78-84.
[15] 张继庆,李汝宁,官举铭,等.四川盆地及邻区晚二叠世生物礁[M].成都:四川科学技术出版社,1990:1-188. ZHANG Jiqing,LI Runing,GUAN Juming,et al. The Late Permian reefs of the Sichuan Basin and its adjacent area[M]. Chengdu:Sichuan Science and Technology Publishing House, 1990:1-188.
[16] 陆廷清,文应初,强子同.中国南方二叠纪海绵礁的成礁模式[J].古生物学报,1998,37(4):513-516. LU Tingqing,WEN Yingchu,QIANG Zitong. Reef-building model of Permian sponge reefs in south China[J]. Acta Palae- ontologica Sinica,1998,37(4):513-516.
[17] 吴熙纯,刘效增,杨仲伦,等.川东上二叠统长兴组生物礁控储层的形成[J].石油与天然气地质,1990,11(3):283-297. WU Xichun,LIU Xiaozeng,YANG Zhonglun,et al. Formation of reef-bound reservoirs of Upper Permian Changxing Forma- tion in east Sichuan[J]. Oil & Gas Geology,1990,11(3):283- 297.
[18] 马永生,牟传龙,郭彤楼,等.四川盆地东北部长兴组层序地层与储层分布[J].地学前缘,2005,12(3):179-185. MA Yongsheng,MU Chuanlong,GUO Tonglou,et al. Sequence stratigraphy and reservoir distribution of the Changxing Formation in northeastern Sichuan Basin[J]. Earth Science Frontiers,2005,12(3):179-185.
[19] 马永生,牟传龙,郭旭升,等.四川盆地东北部长兴期沉积特征与沉积格局[J].地质论评,2006,52(1):25-31. MA Yongsheng,MU Chuanlong,GUO Xusheng,et al. Charac- teristic and framework of the Changxingian sedimentation in the northeastern Sichuan Basin[J]. Geological Review,2006, 52(1):25-31.
[20] 马永生,牟传龙,谭钦银,等.达县-宣汉地区长兴组-飞仙关组礁滩相特征及其对储层的制约[J]. 地学前缘,2007,14(1):182-192. MA Yongsheng,MU Chuanlong,TAN Qinyin,et al. Reef-bank features of Permian Changxing Formation and Triassic Feixian- guan Formation in the Daxian-Xuanhan area,Sichuan prov-ince,south China and constraint for the reservoirs of natural gas[J]. Earth Science Frontiers,2007,14(1):182-192.
[21] 马永生,储昭宏.普光气田台地建造过程及其礁滩储层高精度层序地层学研究[J].石油与天然气地质,2008,29(5):548- 556. MA Yongsheng,CHU Zhaohong. Building-up process of car- bonate platform and high -resolution sequence stratigraphy of reservoirs of reef and oolitic shoal facies in Puguang gas field[J]. Oil & Gas Geology,2008,29(5):548-556.
[22] 周刚,郑荣才,王炯,等.川东-渝北地区长兴组礁、滩相储层预测[J]. 岩性油气藏,2009,21(1):15-21. ZHOU Gang,ZHENG Rongcai,WANG Jiong,et al. Reef and shoal facies reservoir prediction of Changxing Formation in eastern Sichuan and northern Chongqing[J]. Lithologic Reser- voirs,2009,21(1):15-21.
[23] 周刚,郑荣才,罗韧,等.环开江-梁平海槽长兴组生物礁类型及储层特征[J]. 岩性油气藏,2013,25(1):81-87. ZHOU Gang,ZHENG Rongcai,LUO Ren,et al. Types and characteristics of reefs of Permian Changxing Formation around Kaijiang-Liangping trough,eastern Sichuan Basin[J]. Lithologic Reservoirs,2013,25(1):81-87.
[24] 李小燕,王琪,张瑞,等.川东北地区上二叠统盘龙洞生物礁储层特征及其主控因素分析[J]. 天然气地球科学,2011,20(1):63-69. LI Xiaoyan,WANG Qi,ZHANG Rui,et al. Reservoir charac- teristics and main controlling factors of Upper Permian Pan- longdong organic reefs in northeastern Sichuan[J]. Natural Gas Geoscience,2011,20(1):63-69.
[25] 黄仁春,邢凤存,范小军,等.四川盆地元坝地区长兴组-飞仙关组高精度层序地层格架的建立及礁滩储集层预测[J].古地理学报,2019,21(2):369-378. HUANG Renchun,XING Fengcun,FAN Xiaojun,et al. Estab- lishment of high-precision sequence stratigraphic framework of the Changxing-Feixiangguan Formations and prediction of reefshoal reservoir in Yuanba area,Sichuan Basin[J]. Journal of Palaeogeography(Chinese Edition),2019,21(2):369-378.
[26] PERRI E,TUCKER M E,SŁOWAKIEWICZ M,et al. Carbon- ate and silicate biomineralization in a hypersaline microbial mat(Mesaieed sabkha,Qatar):Roles of bacteria,extracellular polymeric substances and viruses[J]. Sedimentology,2018,65(4),1213-1245.
[27] ARVIDSON R S,MACKENZIE F T. The dolomite problem:Control of precipitation kinetics by temperature and saturation state[J]. American Journal of Science,1999,299(4):257-288.
[28] WARREN J. Dolomite:Occurrence,evolution and economically important associations[J]. Earth-Science Reviews,2000,52(1/2/3):1-81.
[29] LAND L S. The origin of massive dolomite[J]. Journal of Geo- logical Education,1985,33(2):112-125.
[30] WEYL P K. Porosity through dolomitization:Conservation of mass requirements[J]. Journal of Sedimentary Petrology,1960, 30(1):85-90.
[31] 黄成刚,王建功,吴丽荣,等.古近系湖相碳酸盐岩储集特征与含油性分析:以柴达木盆地英西地区为例[J].中国矿业大学学报,2017,46(5):909-922. HUANG Chenggang,WANG Jiangong,WU Lirong,et al. Characteristics of lacustrine carbonate reservoirs in Paleogene and oil-bearing property analysis:A case study of the Yingxi area from the western Qaidam Basin[J]. Journal of China University of Mining & Technology,2017,46(5):909-922.
[32] 史建南,郑荣才,冯青平,等.川东北长兴组埋藏白云石化流体来源与油气倒灌式成藏[J].天然气工业,2009,29(3):5-8. SHI Jiannan,ZHENG Rongcai,FENG Qingping,et al. Fluid origin of burial dolomitization and hydrocarbon accumulation model of backward charging in Changxing Formation,NE Sichuan Basin[J]. Natural Gas Industry,2009,29(3):5-8.
[33] 章宇路,文华国,郑荣才,等.川东北铁山-双家坝地区长兴组白云岩成因[J].岩性油气藏,2016,28(5):34-43. ZHANG Yulu,WEN Huaguo,ZHENG Rongcai,et al. Genesis of dolomite of Changxing Formation in Tieshan-Shuangjiaba ar- ea,northeast Sichuan Basin[J]. Lithologic Reservoirs,2016,28(5):34-43.
[34] AZMY K,LAVOIE D,WANG Z R,et al. Magnesium-isotope and REE compositions of Lower Ordovician carbonates from eastern Laurentia:Implications for the origin of dolomites and limestones[J]. Chemical Geology,2013,356:64-75.
[35] KACZMAREK S E,SIBLEY D F. Direct physical evidence of dolomite recrystallization[J]. Sedimentology,2014,61:1862- 1882.
[36] ALLAN J R,WIGGINS W D. Dolomite reservoirs:Geochemi- cal techniques for evaluating origin and distribution[M]. Tulsa:AAPG,1993:36-129.
[37] FAIRBRIDGE R W. The dolomite question[M]//LE BLANC R J,BREEDING J G. Regional aspects of carbonate deposition. Tulsa:SEPM Society for Sedimentary Geology,1957:125-178.
[38] BADIOZAMANI K. The dorag dolomitization model,applica- tion to the middle Ordovician of Wisconsin[J]. Journal of Sedi- mentary Research,1973,43(4):965-984.
[39] ROBERTS J A,KENWARD P A,FOWLE D A,et al. Surface chemistry allows for abiotic precipitation of dolomite at low temperature[J]. Proceedings of the National Academy of Sci- ences of the United States of America,2013,110(36):14540- 14545.
[40] PERTRASH D A,BIALIK O M,BONTOGMALI T R R,et al. Microbially catalyzed dolomite formation:from near-surface to burial[J]. Earth-Science Review,2017,171:558-582.
[41] LAND L S,ZENGER D L,DUNHAM J B,et al. The isotopic and trace element geochemistry of dolomite:The state of the art[M]//Concepts and models of dolomitization. Tulsa:SEPM So- ciety for Sedimentary Geology,1980:87-110.
[42] LAND L S. Failure to precipitate dolomite at 25℃ from dilute solution despite 1000-fold over saturation after 32 years[J]. Aquatic Geochemistry,1998,4:361-368.
[43] LAND L S. Holocene meteoric dolomitization of Pleistocene limestones,North Jamaica[J]. Sedimentology,1973,20:411- 424.
[44] FOLK R L,LAND S. Mg/Ca ratio and salinity:Two controls over crystalization of dolomite[J]. AAPG Bulletin,1975,59(1):60-68.
[45] WARREN J K. Sulfate dominated sea-marginal and platform evaporative settings//MELVIN J L. Evaporites,petroleum and mineral resources[M]. New York:Elsevier Science,1991:477-533.
[46] LUMSDEN D N,CAUDLE G C. Origin of massive dolostone:The Upper Knox model[J]. Journal of Sedimentary Research, 2001,71(3):400-409.
[47] NING Meng,LANG Xianguo,HUANG Kangjun,et al. To- wards understanding the origin of massive dolostones Honglin Yuan[J]. Earth and Planetary Science Letters,2020,545(1):1-8.
[48] ROBERTS J A,BENNETT P C,GOMZALEZ L A,et al. Mi- crobial precipitation of dolomite in methanogenic groundwater[J]. Geology,2004,32(4):277-280.
[49] SÁNCHEZ-ROMÁN M,VASCONCELOS C,SCHMID T,et al. Aerobic microbial dolomite at the nanometer scale:Implica- tions for the geologic record[J]. Geology,2008,36(11):879- 882.
[50] VASCONCELOS C,MCKENZIE J A,WARTHMANN R,et al. Calibration of the δ18 O paleothermometer for dolomite pre- cipitated in microbial cultures and natural environments[J]. Geology,2005,33(4):317-320.
[51] KRAUSE S,LIEBETRAU V,GORB S,et al. Microbial nucle- ation of Mg-rich dolomite in exopolymeric substances under an- oxic modern seawater salinity:New insight into an old enigma[J]. Geology,2012,40(7):587-590.
[52] KACZMAREK S E,GREGG J M,BISH D L,et al. Dolomite, very high-magnesium calcite,and microbes:Implications for the microbial model of dolomitization[M]//MACNEIL A J, LONNEE J,WOOD R. Characterization and modeling of car- bonates:Mountjoy symposium 1. Tulsa:SEPM Society for Sed- imentary Geology,2017:1-14.
[53] SUN S Q,ESTEBAN M. Paleoclimatic controls on sedimenta- tion,diagenesis,and reservoir quality:Lessons from Miocene carbonates[J]. AAPG Bulletin,1994,78(4):519-543.
[54] WRIGHT D T. Benthic microbial communities and dolomite formation in marine and lacustrine environments:A new dolo- mite model[M]//GLENN C R,PREVOT L L,LUCAS J. Ma- rine authigenesis from global to microbial. Tulsa:SEPM Soci- ety for Sedimentary Geology,2000:7-20.
[55] WRIGHT D T,WACY D. Sedimentary dolomite:A reality check[M]//BRAITHWAITE C J R,RIZZI G,DARKE G. The geometry and petrogenesis of dolomite hydrocarbon reservoirs. London:Geological Society of London,2004:65-74.
[56] WRIGHT D T,WACY D. Precipitation of dolomite using sul- phate-reducing bacteria from the Coorong region,South Austra- lia:Signifificance and implications[J]. Sedimentology,2005, 52(5):987-1008.
[57] KATHLEEN C B,ROBERT H G,BRIGITTE W,et al. Ex- tremely acid Permian lakes and ground waters in North America[J]. Nature,1998,30:911-914.
[58] 韩定坤,傅恒,刘雁婷. 白云石化作用对元坝地区长兴组储层发育的影响[J]. 天然气工业,2011,31(10):22-26. HAN Dingkun,FU Heng,LIU Yanting. Effect of dorag dolomi- tization on the development of reservoirs in the Changxing Fm in the Yuanba area[J]. Natural Gas Industry,2011,31(10):22- 26.
[59] SALLER A H,HENDERSON N. Distribution of porosity and permeability in platform dolomites:Insight from the Permian of West Texas[J]. AAPG Bulletin,1998,82(8):1528-1550.
[60] 杨俊杰,黄思静,张文正,等.表生和埋藏成岩作用的温压条件下不同组成碳酸盐岩溶蚀成岩过程的实验模拟[J].沉积学报,1995,13(4):49-54. YANG Junjie,HUANG Sijing,ZHANG Wenzheng,et al. Experimental simulation of dissolution for carbonate with different composition under the conditions from Epigenesis to burial dia- genesis environment[J]. Acta Sedimentologica Sinica,1995,13(4):49-54.
[61] SUN S Q. Dolomite reservoirs:Porosity evolution and reser- voir characteristics[J]. AAPG Bulletin,1995,79(2):186-204.
[62] SEARS S O,LUCIA F J. Dolomitization of northern Michigan Niagara reefs by brine refluxion and freshwater/seawater mixing[M]//ZENGER D L,DUNHAM J B,ETHINGTON R L. Con- cepts and models of dolomitization. Tulsa:SEPM Society for Sedimentary Geology,1980:215-236.
[63] BRAITHWAITE C J R,RIZZI G,DARKE G. The geometry and petrogenesis of dolomite hydrocarbon reservoirs:Introduc- tion[M]. London:Geological Society of London,2018:1-6.
[64] PATTERSON R J,KINSMAN D J J. Formation of diagenetic dolomite in coastal sabkhas along the Arabian(Persian)Gulf[J]. AAPG Bulletin,1982,66(1):28-43.
[65] SCHMOKER J W,KRYSTINNIK K B,HALLER R B. Select- ed characteristics of limestone and dolomite reservoirs in the United States[J]. AAPG Bulletin,1985,69(5):733-741.
[66] MACHEL H G. Concepts and models of dolomitization:A criti- cal reappraisal[M]//BRAITHWAITE C J R,RIZZI G,DARKE G. The geometry and petrogenesis of dolomite hydrocarbon reservoirs. London:Geological Society of London,2004:7-63.
[67] BATHURST R G C. Carbonate sediments and their diagenesis[M]. Amsterdam:Elsevier Scientific Publishing,1975:658.
[68] ROEHL P O. Dilation breciation:Proposed mechanism of frac- turing,petroleum expulsion and dolomitization in the monterey Formation,California[J]. AAPG Bulletin,1979,63(9):1586.
[69] KEITH B D,WICKSTROM L H. Lima-Indiana Trend-U.S.A. Cincinnati and Findlay Arches,Ohio and Indiana[R]. Ohio Geological Survey Columbus,Ohio,1992.
[70] DAVIES G R,SMITH L B. Structurally controlled hydrother- mal dolomite reservoir facies:An overview[J]. AAPG Bulle- tin,2006,90(11):1641-1690.
[71] SMITH L B,DAVIES G R. Implications for the geologic re- cord Structurally controlled hydrothermal alteration of carbon- ate reservoirs:Introduction[J]. AAPG Bulletin,2006,90(11):1635-1640.
[72] REIMER J D,TEARE M R. Deep burial diagenesis and porosity modification in carbonate rocks by thermal-organic sulphate reduction and hydrothermal dolomitization:TSRHTD[R]// HUTCHEON I E,REIMER J,TEARE M,et al. Subsurface dis- solution porosity in carbonates:Recognition,causes and impli- cations. Canadian Society of Petroleum Geologists Short Course Notes,1992.
[73] AL-AASM I S,WHITE T. Mississippian hydrothermal dolomi- tization of the upper Debolt Formation,Sikanni gas field,north- eastern British Columbia(abs.)[C]. Geological Association of Canada,Mineralogical Association of Canada,Annual meeting, 1999.
[74] SMITH L B. Origin and reservoir characteristics of Upper Or- dovician Trenton:Black River hydrothermal dolomite reser- voirs in New York[J]. AAPG Bulletin,2006,90(11):1691- 1718.
[75] SUDRIE M B,CALINE M A,LOPEZ-HORGUE,et al. Faultrelated hydrothermal dolomites in Cretaceous platform carbon- ates from the Karrantza area(north Spain):Outcrop analogues for dolomite reservoir characterization[C]. Bahrain:The 7th Middle East Geosciences Conference and Exhibition,2006.
[76] QING Hairuo,MOUNTJOY E W. Formation of Coarsely Crys- talline,Hydrothermal Dolomite Reservoirs in the Presqu'ile Barrier,Western Canada Sedimentary Basin[J]. AAPG Bulle- tin,1994,78(1):55-77.
[77] 谭秀成,罗冰,江兴福,等. 四川盆地基底断裂对长兴组生物礁的控制作用研究[J].地质论评,2012,58(2):277-284. TAN Xiucheng,LUO Bing,JIANG Xingfu,et al. Controlling effect of basement fault on Changxing Formation reef in Sichuan Basin[J]. Geological Review,2012,58(2):277-284.
[78] 雷卞军,强子同,文应初.川东及邻区上二叠统生物礁一的白云岩化[J].地质论评,1993,40(3):534-544. LEI Bianjun,QIANG Zitong,WEN Yingchu. Dolomitization of the Upper Permian organic reefs in eastern Sichuan and its adjacent areas[J]. Geological Review,1993,40(3):534-544.
[79] 李春荣,潘继平,刘占红.世界大油气田形成的构造背景及其对勘探的启示[J]. 海洋石油,2007,27(3):33-40. LI Chunrong,PAN Jiping,LIU Zhanhong. Tectonic setting of the world's giant oil and gas fields and its revelation for hydro- carbon exploration[J]. Offshore Oil,2007,27(3):33-40.
[80] MILDREXLER D J,ZHAO Maosheng,RUNNIING S W. Sat- ellite finds highest land skin temperatures on Earth[J]. Bulletin of the American Meteorological Society,2011,92(7):855-860.
[81] ZAMBITOIV J J,BENISON K C. Extremely high tempera- tures and paleoclimate trends recorded in Permian ephemeral lake halite[J]. Geology,2013,41(5):587-590.
[82] CHEN Bo,JOACHIMSKI M M,SHEN Shuzhong,et al. Permian ice volume and palaeoclimate history:Oxygen isotope proxies revisited[J]. Gondwana Research,2013,24(1):77-89.
[83] 李江海,姜洪福.全球古板块再造、岩相古地理及古环境图集[M].北京:地质出版社,2013:32-36. LI Jianghai,JIANG Hongfu. Global atlas of Paleoplate recon- struction,lithofacies paleogeography and Paleoenvironment[M]. Beijing:Geological Publishing House,2013:32-36.
[84] KATZ A,MATTHEWS A. The dolomitization of CaCO3:An experimental study at 252-295℃[J]. Geochimica et Cosmochi- mica Acta,1977,41(2):297-308.
[85] GAINES A M. An experimental investigation of the kinetics and mechanism of the formation of dolomite[D]. Chicago:The University of Chicago,1968.
[86] BURNS S J,MCKENZIE J A,VASCONCELOS C. Dolomite formation and biogeochemical cycles in the Phanerozoic[J]. Sedimentology,2000,47(Suppl 1):49-61.
[87] PARRISH J M. Vertebrate paleoecology of the Chinle Forma- tion(Late Triassic)of the southwestern United States[J]. Pal- aeogeography,Palaeoclimatology,Palaeoecology,1989,72:227- 247.
[88] PARRISH J T,ZIEGLER A M. Permian-Triassic paleogeogra- phy and paleoclimatology and implications for therapsid distri- butions,in Hotton[M]//HOTTON N,MACLEAN P D,ROTH J J,et al. The Ecology and Biology of Mammal-like Reptiles. Washington:Smithsonian Press,1986:109-132.
[89] DIMICHELE W A,TABOR N J,CHANEY D S,et al. From wetlands to wet spots:Environmental tracking and the fate of Carboniferous elements in Early Permian tropical floras[G]// GREB S F,DIMICHELE W A. Wetlands through time. Geo- logical Society of America,2006:223-248.
[1] 张振华, 张小军, 钟大康, 苟迎春, 张世铭. 柴达木盆地西北部南翼山地区古近系下干柴沟组上段储层特征及主控因素[J]. 岩性油气藏, 2023, 35(3): 29-39.
[2] 柳忠泉, 赵乐强, 曾治平, 田继军, 李正强, 罗锦昌, 胡美玲. 准噶尔盆地阜康断裂带二叠系芦草沟组页岩油成藏条件[J]. 岩性油气藏, 2023, 35(3): 126-137.
[3] 江梦雅, 王江涛, 刘龙松, 李卉, 陈海龙, 蒋中发, 王学勇, 刘海磊. 准噶尔盆地盆1井西凹陷石炭系—二叠系天然气特征及成藏主控因素[J]. 岩性油气藏, 2023, 35(3): 138-151.
[4] 卜旭强, 王来源, 朱莲花, 黄诚, 朱秀香. 塔里木盆地顺北油气田奥陶系断控缝洞型储层特征及成藏模式[J]. 岩性油气藏, 2023, 35(3): 152-160.
[5] 方锐, 蒋裕强, 陈沁, 曾令平, 罗宇卓, 周亚东, 杜磊, 杨广广. 川东北五宝场地区侏罗系沙溪庙组沉积特征[J]. 岩性油气藏, 2023, 35(2): 47-58.
[6] 冯明友, 高瑞琪, 王兴志, 徐亮, 赵金, 刘小洪, 尚俊鑫. 川西南宝兴地区二叠系栖霞组一段白云岩储层充填序列及流体指示[J]. 岩性油气藏, 2023, 35(2): 11-20.
[7] 马东烨, 陈宇航, 赵靖舟, 吴伟涛, 宋平, 陈梦娜. 鄂尔多斯盆地东部二叠系下石盒子组8段河流相砂体构型要素[J]. 岩性油气藏, 2023, 35(1): 63-73.
[8] 杨跃明, 张少敏, 金涛, 明盈, 郭蕊莹, 王兴志, 韩璐媛. 川南地区二叠系龙潭组页岩储层特征及勘探潜力[J]. 岩性油气藏, 2023, 35(1): 1-11.
[9] 曾治平, 柳忠泉, 赵乐强, 李艳丽, 王超, 高平. 准噶尔盆地西北缘哈山地区二叠系风城组页岩油储层特征及其控制因素[J]. 岩性油气藏, 2023, 35(1): 25-35.
[10] 李凌, 张照坤, 李明隆, 倪佳, 耿超, 唐思哲, 杨文杰, 谭秀成. 四川盆地威远—高石梯地区二叠系栖霞阶层序地层特征及有利储层分布[J]. 岩性油气藏, 2022, 34(6): 32-46.
[11] 米伟伟, 谢小飞, 曹红霞, 马强, 杜永慧, 张琼, 邓长生, 宋珈萱. 鄂尔多斯盆地东南部二叠系山2—盒8段致密砂岩储层特征及主控因素[J]. 岩性油气藏, 2022, 34(6): 101-117.
[12] 杨帆, 卞保力, 刘慧颖, 姚宗全, 尤新才, 刘海磊, 卫延召. 玛湖凹陷二叠系夏子街组限制性湖盆扇三角洲沉积特征[J]. 岩性油气藏, 2022, 34(5): 63-72.
[13] 罗锦昌, 田继军, 马静辉, 闫嘉启, 梁雅菲, 胡卓浩. 吉木萨尔凹陷吉页1井区二叠系芦草沟组沉积环境及有机质富集机理[J]. 岩性油气藏, 2022, 34(5): 73-85.
[14] 吕正祥, 廖哲渊, 李岳峰, 宋修章, 李响, 何文军, 黄立良, 卿元华. 玛湖凹陷二叠系风城组碱湖云质岩储层成岩作用[J]. 岩性油气藏, 2022, 34(5): 26-37.
[15] 阴钰毅, 姚志纯, 郭小波, 王乐立, 陈思谦, 余小雷, 岑向阳. 鄂尔多斯盆地西缘二叠系隐伏构造特征及勘探意义[J]. 岩性油气藏, 2022, 34(4): 79-88.
Viewed
Full text


Abstract

Cited

  Shared   
  Discussed   
[1] 黄思静,黄培培,王庆东,刘昊年,吴 萌,邹明亮. 胶结作用在深埋藏砂岩孔隙保存中的意义[J]. 岩性油气藏, 2007, 19(3): 7 -13 .
[2] 丁超,郭兰,闫继福. 子长油田安定地区延长组长6 油层成藏条件分析[J]. 岩性油气藏, 2009, 21(1): 46 -50 .
[3] 李彦山,张占松,张超谟,陈鹏. 应用压汞资料对长庆地区长6 段储层进行分类研究[J]. 岩性油气藏, 2009, 21(2): 91 -93 .
[4] 罗 鹏,李国蓉,施泽进,周大志,汤鸿伟,张德明. 川东南地区茅口组层序地层及沉积相浅析[J]. 岩性油气藏, 2010, 22(2): 74 -78 .
[5] 潘建国,卫平生,张虎权,谭开俊. 地震储层学与相关学科的比较[J]. 岩性油气藏, 2010, 22(3): 1 -4 .
[6] 左国平,屠小龙,夏九峰. 苏北探区火山岩油气藏类型研究[J]. 岩性油气藏, 2012, 24(2): 37 -41 .
[7] 邢二涛,张云锋. 水平井开发技术在贝中区N1 段应用研究[J]. 岩性油气藏, 2010, 22(Z1): 93 -95 .
[8] 王飞宇. 提高热采水平井动用程度的方法与应用[J]. 岩性油气藏, 2010, 22(Z1): 100 -103 .
[9] 袁云峰,才业,樊佐春,姜懿洋,秦启荣,蒋庆平. 准噶尔盆地红车断裂带石炭系火山岩储层裂缝特征[J]. 岩性油气藏, 2011, 23(1): 47 -51 .
[10] 袁剑英,付锁堂,曹正林,阎存凤,张水昌,马达德. 柴达木盆地高原复合油气系统多源生烃和复式成藏[J]. 岩性油气藏, 2011, 23(3): 7 -14 .