Liu Wei, Huang Qing-yu, Wang Kun, Shi Shu-yuan . Dolomization and influence on reservoir development in deep-burial stage:A case study of Lower Paleozoic in Tarim Basin[J]. Natural Gas Geoscience, 2016 , 27(5) : 772 -779 . DOI: 10.11764/j.issn.1672-1926.2016.05.0772

[1]Qiang Zitong.Reservoir Geology of the Carbonate Rocks[M].Dongying:Petroleum University Publishing House,1998:336-380.[强子同.碳酸盐岩储层地质学[M].东营:石油大学出版社,1998:336-380.]
[2]Huang Sijing.Diagenesis of Carbonate[M].Beijing:Geological Publishing House,2010:177-180.[黄思静.碳酸盐岩的成岩作用[M].北京:地质出版社,2010:177-180.]
[3]Dunnington H V.Aspects of Diagenesis and Shape Change in Stylolitic Limestone Reservoirs[M].New York,Elsevier:Proceedings of the Seventh World Petroleum Congress(Mexico City,Mexico).1967:339-352.
[4]Neugebauer J.Some Aspects of Cementation in Chalk.Pelagic Sediments:On Land and Under the Sea[M].Oxford:International Association of Sedimentologists Special Publication,1974:149-176.
[5]Buxton T M,Sibley D F.Pressure solution features in a shallow buried limestone[J].Journal of Sedimentary Petrology,1981,51(1):19-26.
[6]Allan J R,Wiggins W D.Dolomite Reservoirs:Geochemical Techniques for Evalution Origin and Distribution[M].Tulsa,1994.
[7]Qiang Zitong,Zeng Deming,Wang Xingzhi,et al.Isotopic geochemical characteristics of oolitic bank dolostones in the Lower Triassic Feixianguan Formation in northeastern Sichuan Province[J].Journal of Palaeogeoraphy,2012,14(3):13-20.[强子同,曾德铭,王兴志,等.川东北下三叠统飞仙关组鲕粒滩白云岩同位素地球化学特征[J].古地理学报,2012,14(3):13-20.]
[8]Zhang Yongsheng.Mechanism of deep burial dolomitization of massive dolostones in the Middle Majiagou Group of the Ordovician,Ordos Basin[J].Acta Sedimentologica Sinica,2000,18(3):424-430.[张永生.鄂尔多斯地区奥陶系马家沟群中部块状白云岩的深埋藏白云石化机制[J].沉积学报,2000,18(3):424-430.]
[9]Yi Haisheng,Chen Zhiyong,Ji Changju,et al.New evidence for deep burial origin of sucrosic dolomites from Middle Jurrasic Buqu Formation in southern Qiangtang Basin[J].Acta Petrologica Sinica,2014,30(3):737-746.[伊海生,陈志勇,季长军,等.羌塘盆地南部地区布曲组砂糖状白云岩埋藏成因的新证据[J].岩石学报,2014,30(3):737-746.]
[10]Zhao Wenzhi,Shen Anjiang,Hu Suyun.et al.Types and distributional features of Cambrian-Ordovician dolostone reservoirs in Tarim Basin,northwestern China[J].Acta Petrologica Sinica,2012,28(3):758-76.[赵文智,沈安江,胡素云,等.塔里木盆地寒武—奥陶系白云岩储层类型与分布特征[J].岩石学报,2012,28(3):758-76.]
[11]Lin Jun,Zhou Fangfang,Yuan Guofen.Features of deep-burial dolomitization of the Cambrian reservoirs in Tahe region[J].Oil & Gas Geology,2010,31(1):13-27.[蔺军,周芳芳,袁国芬.塔河地区寒武系储层深埋藏白云石化特征[J].石油与天然气地质,2010,31(1):13-27.]
[12]Liu Wei,Zhang Guangya,Pan Wenqing,et al.Lithofacies Palaeogeography of the Cambrian in Tarim Basin[J].Journal of Palaeogeoraphy,2011,13(5):529-538.[刘伟,张光亚,潘文庆,等.塔里木地区寒武纪岩相古地理及沉积演化[J].古地理学报,2011,13(5):529-538.]
[13]Liu Wei,Zhang Xingyang,Gu Jiayu.Sedimentary environment of Lower-Middle Ordovician Yingshan Formation in mid-western Tarim Basin[J].Acta Sedimentologica Sinica ,2009,27(3):435-442.[刘伟,张兴阳,顾家裕.塔里木盆地台盆区中西部中下奥陶统鹰山组沉积环境研究[J].沉积学报,2009,27(3):435-442.]
[14]Zheng Jianfeng,Shen Anjiang,Liu Yongfu,et al.Multi-parameter comprehensive identification of the genesis of Lower Paleozoic dolomite in Tarim Basin,China[J].Acta Petrolei Sinica,2012,33(supplement2):145-153.[郑剑锋,沈安江,刘永福,等.多参数综合识别塔里木盆地下古生界白云岩成因[J].石油学报,2012,33(增刊2):145-153.]
[15]Ma Feng,Xu Huaixian,Gu Jiayu,et al.Cambrian dolomite origin and reservoir evolution in east Tarim Basin[J].Petroleum Exploration and Development,2009,36(2):143-155.[马峰,许怀先,顾家裕,等.塔东寒武系白云岩成因及储层演化特征[J].石油勘探与开发,2009,36(2):143-155.]
[16]Gu Jiayu.Characteristics and origin analysis of dolomite in Lower Ordovician of Tarim Basin[J].Xinjiang Petroleum Geology,2000,21(2):120-122.[顾家裕.塔里木盆地下奥陶统白云岩特征及成因[J].新疆石油地质,2000,21(2):120-122.]
[17]Jin Zhenkui,Yang Youxing,Yu Kuanhong.Genetic types of dolostones in the Cambrian,eastern Tarim Basin[J].Journal of Palaeogeoraphy,2012,14(6):747-756.[金振奎,杨有星,余宽宏,等.塔里木盆地东部地区寒武系白云岩成因类型[J].古地理学报,2012,14(6):747-756.]
[18]Huang Wenhui,Wang Anjia,Wan Huan,et al.Discussion on characteristics of the Cambrian-Ordovician carbonate rocks reservoirs and origin of dolostones in Tarim Basin[J].Journal of Palaeogeoraphy,2012,14(2):197-208.[黄文辉,王安甲,万欢,等.塔里木盆地寒武-奥陶系碳酸盐岩储集特征与白云岩成因探讨[J].古地理学报,2012,14(2):197-208.]
[19]Zheng Jianfeng,Shen Anjiang,Liu Yongfu,et al.Genesis and distribution of the Cambro-Ordovician dolomite in Tarim Basin[J].Xinjiang Petroleum Geology,2011,32(6):600-604.[郑剑锋,沈安江,刘永福,等.塔里木盆地寒武—奥陶系白云岩成因及分布规律[J].新疆石油地质,2011,32(6):600-604.]
[20]Li Pengchun,Chen Guanghao,Zeng Qiaosong,et al.Genesis of Lower Ordovician dolomite in central Tarim Basin[J].Acta Sedimentologica Sinica,2011,29(5):842-856.[李鹏春,陈广浩,曾乔松,等.塔里木盆地塔中地区下奥陶统白云岩成因[J].沉积学报,2011,29(5):842-856.]
[21]Zheng Jianfeng,Shen Anjiang,Qiao Zhanfeng,et al.Genesis of dolomite and main controlling factors of reservoir in Penglaiba Formation of Lower Ordovician,Tarim Basin:A case study of Dabantage outcrop in Bachu area[J].Acta Petrologica Sinica,2013,29(9):3223-3232.[郑剑锋,沈安江,乔占峰,等.塔里木盆地下奥陶统蓬莱坝组白云岩成因及储层主控因素分析——以巴楚大班塔格剖面为例[J].岩石学报,2013,29(9):3223-3232.]
[22]Zhan Demin,Bao Zhidong,Pan Wenqing,et al.Type and origin of the Lower Paleozoic dolostones in Tarim Basin[J].Journal of Palaeogeoraphy,2013,15(5):693-706.[张德民,鲍志东,潘文庆,等.塔里木盆地下古生界白云岩类型及成因[J].古地理学报,2013,15(5):693-706.]
[23]He Ying,Bao Zhidong,Shen Anjiang,et al.The genetic mechanism of dolostones of the Cambrian-Lower Ordovician in Yaha-Yingmaili region,Tarim Basin[J].Acta Sedimentologica Sinica,2006,24(6):806-818.[何莹,鲍志东,沈安江,等.塔里木盆地牙哈—英买力地区寒武系—下奥陶统白云岩形成机理[J].沉积学报,2006,24(6):806-818.]
[24][JP2]Budd D A.Cenozoic dolomites of carbonate islands:their attributes and origin[J].Earth-Science Review,1997,42(1):1-47.[JP]
[25]Veizer J.Strontium isotopes in seawater through time[J]:Geochimica et Cosmochimica Acta,1989,53(11):141-167.
[26]Veizer J,Ala D,Azmy K,et al.87Sr/86Sr,δ13C and δ18O evolution of Phanerozoic seawater[J].Chemical Geology,1999,161(1):59-88.
[27]Qing H,Mountjoy E W.Origin of dissolution vugs,caverns,and breccias in the Middle Devonian Presqu'ile barrier,host of Pine Point MVT deposits[J].Economic Geology,1994,89(4):858-876.
[28]Katz D A,Eberli G P,Swart P K,et al.Tectonic-hydrothermal brecciation associated with calcite precipitation and permeability destruction in Mississippian carbonate reservoirs,Montana and Wyoming[J].AAPG Bulletin,2006,90(11):1803-1841.
[29]Lonnee J,Machel H G.Pervasive dolomitization with subsequent hydrothermal alteration in the Clarke Lake gas field,Middle Devonian Slave Point Formation,British Columbia,Canada[J].AAPG Bulletin,2006,90(11):1739-1761.
[30]Chen Daizhao.Structure-controlled hydrothermal dolomization and hydrothermal dolomite reservoirs[J].Oil & Gas Geology,2008,29(5):614-622.[陈代钊.构造—热液白云岩化作用与白云岩储层[J].石油与天然气地质,2008,29(5):614-622.]
[31]Cai C,Franks S G,Aagaard P.Origin and migration of brines from Paleozoic strata in central Tarim,China:constraints from87Sr/86Sr,δD,δ18O and water chemistry[J].Applied Geochemistry,2001,16(9):1269-1284.
[32]Cai C,Li K,Li H,et al.Evidence for cross formational hot brine flow from integrated87Sr/86Sr,REE and fluid inclusions of the Ordovician veins in central Tarim,China[J].Applied Geochemistry,2008,23(8):2226-2235.
[33]Ｈuang Ｑingyu,Zhang Shaonan,Zhang Siyang,et al.Textural control on the development of dolomite reservori:A study from the Cambrian-Ordovician dolomite,central Tarim Basin,NW China[J].Nature Gas Geoscience,2014,25(3):341-350.[黄擎宇,张哨楠,张斯杨,等.白云岩结构对储集空间发育的控制作用——以塔里木盆地中央隆起区寒武系—奥陶系白云岩为例[J].天然气地球科学,2014,25(3):341-350.]