[1]Burne,Moore.Microbialites:Organosedimentary deposits of benthic microbial communities[J].Palaios,1987(2):241-254.
[2]Riding R.Microbial carbonates:The geological record of calcified bacterial-algal mats and biofilms[J].Sedimentology,2000,47(supplement 1):179-214.
[3]Li Pengwei,Luo Ping,Chen Min,et al.Characteristics and origin of the Upper Sinian microbial carbonate reservoirs at the northwestern margin of Tarim Basin[J].Oil & Gas Geology,2015,36(3):416-428.[李朋威,罗平,陈敏,等.塔里木盆地西北缘上震旦统微生物碳酸盐岩储层特征与成因[J].石油与天然气地质,2015,36(3):416-428.
[4]Luo Ping,Wang Shi,Li Pengwei,et al.Review and prospectives of microbial carbonate reservoirs[J].Acta Sedimentologica Sinica,2013,31(5):807-823.[罗平,王石,李朋威,等.微生物碳酸盐岩油气储层研究现状与展望[J].沉积学报,2013,31(5):807-823.]
[5]Fang Shaoxian,Hou Fanghao,Dong Zhaoxiong.Non-stromatolite ecologic system cyanobacteria dolostone in Dengying Formation of Upper Sinian[J].Acta Sedimentology Sinica,2003,21(1):96-105.[方少仙,侯方浩,董兆雄.上震旦统灯影组中非叠层石生态系兰细菌白云岩[J].沉积学报,2003,21(1):96-105.]
[6]Wei Guoqi,Yang Wei,Du Jinhu,et al.Geological characteristics of the Sinian-Early Cambrian intracratonic rift,Sichuan Basin[J].Natural Gas Industry,2015,35(1):24-35.[魏国齐,杨威,杜金虎,等.四川盆地震旦纪一早寒武世克拉通内裂陷地质特征[J].天然气工业,2015,35(1):24-35.]
[7]Li Jianghai,Jiang Hongfu.Global Ancient Plate Reengineering,Lithofacies Paleogeographic and Paleo-environment Atlas[M].Beijing:Geology Publishing House,2013.[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.]
[8]Li Zongyin,Jiang Hua,Wang Zecheng,et al.Control of tectonic movement on hydrocarbon accumulation in the Sinian strata,Sichuan Basin[J].Natural Gas Industry,2014,34(3):23-30.[李宗银,姜华,汪泽成,等.构造运动对四川盆地震旦系油气成藏的控制作用[J].天然气工业,2014,34(3):23-30.]
[9]Jiang Hua,Wang Zecheng,Du Hongyu,et al.Tectonic evolution of the Leshan-Longnvsi paleo-uplift and reservoir formation of Neoproterozoic Sinian gas[J].Natural Gas Geoscience,2014,25(2):192-200.[姜华,汪泽成,杜宏宇,等.乐山 龙女寺古隆起构造演化与新元古界震旦系天然气成藏[J].天然气地球科学,2014,25(2):192-200.]
[10]Wei Guoqi,Yang Wei,Du Jinhu,et al.Tectonic features of Gaoshiti-Moxi paleo-uplift and its controls on the formation of a giant gasfield,Sichuan Basin,SW China[J].Petroleum Exploration and Development,2015,42(3):257-265.[魏国齐,杨威,杜金虎,等.四川盆地高石梯一磨溪古隆起构造特征及对特大型气田形成的控制作用[J].石油勘探与开发,2015年,42(3):257-265.]
[11]Awramik S M.Precambrian columnar stromatolite diversity:reflection of metazoan appearance[J].Science,1971,174:825-827.
[12]Monty C L V,Bosence D W J,Bridges P H.Carbonate Mud Mounds:Their Origin and Evolution(Special Publication No.23 of the IAS)[M].London:Wiley-Blackwell,1995:3-9.
[13]Luo Bing,Luo Wenjun,Wang Wenzhi,et al.Formation mechanism of the Sinian natural gas reservoir in the Leshan-Longnvsi Paleo-uplift,Sichuan Basin[J].Natural Gas Geoscience,2015,26(3):444-455.[罗冰,罗文军,王文之,等.四川盆地乐山_龙女寺古隆起震旦系气藏形成机制[J].天然气地球科学,2015,26(3):444-455.]
[14]Zou Caineng,Du Jinhu,Xu Chunchun,et al.Formation distribution resource potential and discovery of the Sinian-Cambrían giant gasfield Sichuan Basin,SW China[J].Petroleum Exploration and Development,2014,41(3):278-293.[邹才能,杜金虎,徐春春,等.四川盆地震旦系_寒武系特大型气田形成分布、资源潜力及勘探发现[J].石油勘探与开发,2014,41(3):278-293.]
[15]Wei Guoqi,Du Jinhu,Xu Chunchun,et al.Characteristics and accumulation modes of large gas reservoirs in Sinian-Cambrian of Gaoshiti-Moxi region,Sichuan Basin[J].Acta Petrolei Sinica,2015,36(1):1-12.[魏国齐,杜金虎,徐春春,等.四川盆地高石梯一磨溪地区震旦系_寒武系大型气藏特征与聚集模式[J].石油学报,2015,36(1):1-12.]
[16]Zhang Lin,Wei Guoqi,Wang Zecheng,et al.Analysis of formation mechanism of Sinian Dengying Formation in Gaoshiti-Moxistructure belt in Sichuan Basin[J].Natural Gas Geoscience,2004,15(6):584-589.[张林,魏国齐,汪泽成,等.四川盆地高石梯一磨溪构造带震旦系灯影组的成藏模式[J].天然气地球科学,2004,15(6):584-589.]
[17]Grotzinger J P, James N P.Carbonate Sedimentation and Diagenesis in the Evolving Precambrian World(Special Publication 67 of the IAS)[M].Tulsa,Oklahoma,U.S.A:SEPM,2000:3-22..
[18][JP3]Awramik S M,Sprinkle J.Proterozoic stromatolites:the first marine evolutionary biota[J].Historical Biology,1999,13(4):241-253.
[19]Kennard J M,James N P.Thrombolites and stromatolites;two distinct types of microbial structures[J].Palaios,1986,1(5):492-500.
[20]Zhou Zheng,Wang Xingzhi,Xie Ling,et al.Reservoir features and physical influences of the Sinian Dengying Formation incentral Sichuan,China[J].Natural Gas Geoscience,2014,25(5):701-708.[周正,王兴志,谢林,等.川中地区震旦系灯影组储层特征及物性影响因素[J].天然气地球科学,2014,25(5):701-708.]
[21]Aitken J D.Classification and environmental significance of cryptalgal limestones and dolomites,with illustrations from the Cambrian and Ordovician of southwest Alberta[J].Journal of Sedimentary Petrology,1967,37(4):1163-1l78.
[22]Mei Mingxiang.Discussion on advances of microbial carbonates from the terminological change of thrombolites[J].Geological Science and Technology Information,2007,26(6):1-9.[梅冥相.从凝块石概念的演变论微生物碳酸盐岩的研究进展[J].地质科技情报,2007,26(6):1-9.]
[23]Zhang Yinben.Preliminary study on the botryoidal structures in the Sinian dolostones[J].Petroleum Geology & Experimental,1980(4):40-43.[张荫本.震旦纪白云岩中的葡萄状构造成因初探[J].石油实验地质,1980(4):40-43.]
[24]Xiang Fang,Hong De,Zhang Jinquan.Studying on the origin of botryoidal lace in dolomitite of Dengying Formation,Sinian from Ziyang Sichuan[J].Journal of Mineral Petrology,1998,18(supplement):136-138.[向芳,洪德,张锦泉.资阳地区震旦系灯影组白云岩中葡萄花边的成因研究[J].矿物岩石,1998,18(增刊):136-138.]
[25]Shi Zhejing,Liang Ping,Wang Yong,et al.Geochemical characteristics and genesis of grapestone in Sinian Dengying Formation in southeastern Sichuan Basin[J].Acta Petrologica Sinica,2011,27 (8):2263-2271.[施泽进,梁平,王勇,等.川东南地区灯影组葡萄石地球化学特征及成因分析[J].岩石学报,2011,27(8):2263-2271.] |