Huang Qing-yu, Hu Su-yun, Pan Wen-qing, Liu Wei, Zhang Yan-qiu, Shi Shu-yuan, Wang Kun . Characteristics and controlling factors of the Cambrian carbonate reservoirs in Bachu area,Tarim Basin,NW China[J]. Natural Gas Geoscience, 2016 , 27(6) : 982 -993 . DOI: 10.11764/j.issn.1672-1926.2016.06.0982

[1]Yang Haijun.Exploration knowledge and direction of Lower Proterozoic[JP] inner dolostones,Tarim Basin[J].Natural Gas Geoscience.2015,26(7):1213-1223.[杨海军.塔里木盆地下古生界内幕白云岩勘探认识与勘探方向[J].天然气地球科学,2015,26(7):1213-1223.]
[2]Wang Zhaoming,Xie Huiwen,Chen Yongquan,et al.Discovery and exploration of Cambrian subsalt dolomite original hydrocarbon reservoir at Well Zhongshen-1 in Tarim Basin[J].China Petroleum Exploration,2014,19(2):1-13.[王招明,谢会文,陈永权,等.塔里木盆地中深1井寒武系盐下白云岩原生油气藏的发现与勘探意义[J].中国石油勘探,2014,19(2):1-13.]
[3][KG*6/7]Cai Xiyao,Mao Shuhua,Qian Yixiong,et al.Stratigraphic classification and correlation of Cambrian in Bachu Uplift,Tarim Basin[J].Xinjiang Petroleum Geology,2009,30(1):38-42.[蔡习尧,毛树华,钱一雄,等.塔里木盆地巴楚隆起寒武系划分与对比[J].新疆石油地质,2009,30(1):38-42.]
[4]Liu Yanting,Fu Heng,Chen Ji,et al.Sequence stratigraphy of Cambrian in Bachu-Tazhong area,Tarim Basin[J].Lithologic Reservoirs,2010,22(2):48-53.[刘雁婷,傅恒,陈骥,等.塔里木盆地巴楚—塔中地区寒武系层序地层特征[J].岩性油气藏,2010,22(2):48-53.]
[5]Liu Zhongbao,Yang Shengbin,Jiao Cunli,et al.High resolution sequence stratigraphy and sedimentary characteristics of the Middle-Lower Cambrian in Bachu Uplift,the Tarim Basin[J].Oil & Gas Geology,2012,33(1):70-76.[刘忠宝,杨圣彬,焦存礼,等.塔里木盆地巴楚隆起中、下寒武统高精度层序地层与沉积特征[J].石油与天然气地质,2012,33(1):70-76.]
[6]Tang Daqing,Chen Honghan,Yun Lu,et al.The differential activity characteristics and its evolution of the faults in the Bachu Uplift,Tarim Basin[J].Chinese Journal of Geology,2014,49(1):49-68.[唐大卿,陈红汉,云露,等.塔里木盆地巴楚隆起断裂差异活动特征及成因演化[J].地质科学,2014,49(1):49-68.]
[7]Lv Haitao,Zhang Zhongpei,Shao Zhibing,et al.Structural evolution and exploration significance of the Early Paleozoic palaeouplifts in Bachu-Maigaiti area,the Tarim Basin[J].Oil & Gas Geology,2010,31(1):76-83,90.[吕海涛,张仲培,邵志兵,等.塔里木盆地巴楚—麦盖提地区早古生代古隆起的演化及其勘探意义[J].石油与天然气地质,2010,31(1):76-83,90.]
[8]Zhang XianJun,Zhu ChangJian,Shi Jun,et al.Characteristics of Ordovician carbonate reservoirs in Hetian River Gasfield and its adjacent areas[J].Natural Gas Geoscience,2008,19(1):120-125.[张现军,朱长见,师骏,等.塔里木盆地和田河气田及其周缘地区奥陶系碳酸盐岩储集层特征探讨[J].天然气地球科学,2008,19(1):120-125.]
[9]Ding Wenlong,Qi Lixin,Yun Lu,et al.The tectonic evolution and its controlling effects on the development of Ordovician reservoir in Bachu-Markit Tarim Basin[J].Acta Petrologica Sinica,2012,28(8):2542-2556.[丁文龙,漆立新,云露,等.塔里木盆地巴楚_麦盖提地区古构造演化及其对奥陶系储层发育的控制作用[J].岩石学报,2012,28(8):2542-2556.]
[10]Zhao Zongju,Luo Jiahong,Zhang Yunbo,et al.Lithofacies paleogeography of Cambrian sequences in the Tarim Basin[J].Acta Petrolei Sinica,2011,32(6):937-948.[赵宗举,罗家洪,张运波,等.塔里木盆地寒武纪层序岩相古地理[J].石油学报,2011,32(6):937-948.]
[11]Song Jinmin,Luo Ping,Yang Shisheng,et al.Reservoirs of Lower Cambrian microbial carbonates,Tarim Basin,NW China[J].Petroleum Exploration and Development,2014,41(4):404-413,437.[宋金民,罗平,杨式升,等.塔里木盆地下寒武统微生物碳酸盐岩储集层特征[J].石油勘探与开发,2014,41(4):404-413,437.]
[12]Xiong Yixue,Chen Yongquan,Guan Baozhu,et al.Distribution of northern platform margin and implications to favorable exploration regions on Lower Cambrian Xiaoerbulake Formation,Tarim Basin[J].Acta Sedimentologica Sinica,2015,33(2):408-415.[熊益学,陈永权,关宝珠,等.塔里木盆地下寒武统肖尔布拉克组北部台缘带展布及其油气勘探意义[J].沉积学报,2015,33(2):408-415.]
[13]Li Baohua,Den Shibiao,Chen Yongquan,et al.The reservoir modeling of platform margin dolostone of Xiaoerblak Formation,Lower Cambrian,Kalpin area,Tarim Basin[J].Natural Gas Geoscience,2015,26(7):1233-1244.[李保华,邓世彪,陈永权,等.塔里木盆地柯坪地区下寒武统台缘相白云岩储层建模[J].天然气地球科学,2015,26(7):1233-1244.]
[14]Baomin Zhang,Jingjiang Liu.Classification and characteristics of karst reservoirs in China and related theories[J].Petroleum Exploration and Development,2009,36(1):12-29.[张宝民,刘静江.中国岩溶储集层分类与特征及相关的理论问题[J].石油勘探与开发,2009,36(1):12-29.]
[15][KG*5/6]Huang Sijing.Carbonate Diagenesis[M].Beijing:Geological Publishing House,2010.[黄思静.碳酸盐岩的成岩作用[M].北京:地质出版社,2010.]
[16]Ehrenberg S N,Walderhaug O,Bjrlykke K.Carbonate porosity creation by mesogenetic dissolution:Reality or illusion[J].AAPG Bulletin,2012,96(2):217-233.
[17]Bjrlykke K,Jahren J.Open or closed geochemical systems during diagenesis in sedimentary basins:Constraints on mass transfer during diagenesis and the prediction of porosity in sandstone and carbonate reservoirs[J].AAPG Bulletin,2012,96(12):2193-2214.
[18]Zhao Wenzhi,Shen Anjiang,Zheng Jianfeng,et al.The porosity origin of dolostone reservoirs in the Tarim,Sichuan and Ordos Basins and its implication to reservoir prediction[J].Science China:Earth Sciences,2014,44(9):1925-1939.[赵文智,沈安江,郑剑锋,等.塔里木、四川及鄂尔多斯盆地白云岩储层孔隙成因探讨及对储层预测的指导意义[J].中国科学:地球科学,2014,44(9):1925-1939.]
[19]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.
[20]Huang Sijing,Qing Hairuo,Hu Zuowei,et al.Closed-system dolomitization and the significance for petroleum and economic geology:An example from Feixianguan carbonates:Triassic,NE Sichuan Basin of China[J].Acta Petrologica Sinica,2007,23(11):2955-2962.[黄思静,Hairuo Qing,胡作维,等.封闭系统中的白云岩化作用及其石油地质学和矿床学意义——以四川盆地东北部三叠系飞仙关组碳酸盐岩为例[J].岩石学报,2007,23(11):2955-2962.]
[21]Huang Qingyu,Zhang Shaonan,Meng Xianghao,et al.Textural types and origin of the Cambrian-Ordovician dolomite in the central Tarim Basin[J].Acta Sedimentologica Sinica,2014,32(3):537-549.[黄擎宇,张哨楠,孟祥豪,等.塔里木盆地中央隆起区寒武—奥陶系白云岩结构特征及成因探讨[J].沉积学报,2014,32(3):537-549.]
[22]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.]
[23]Pu R,Qing H,Kent D M,et al.Pool characterization of Ordovician Midale field:Implication for Red River play in northern Williston basin,southeastern Saskatchewan,Canada[J].AAPG bulletin,2003,87(11):1699.
[24]Gingras M K,Mendoza C A,Pemberton S G.Fossilized worm burrows influence the resource quality of porous media[J].AAPG Bulletin,2004,88(7):875-883.
[25]Pemberton S G,Gingras M K.Classification and characterizations of biogenically enhanced permeability[J].AAPG Bulletin,2005,89(11):1493-1517.
[26]Kendall A C.Origin of dolomite mottling in Ordovicianlimestones from Saskatchewan and Manitoba[J].Bulletin of Canadian Petroleum Geology,1977,25(3):480-504.
[27]Gingras M K,Pemberton S G,Muelenbachs K,et al.Conceptual models for burrow-related,selective dolomitization with textural and isotopic evidence from the Tyndall Stone,Canada[J].Geobiology,2004,2(1):21-30.