微生物碳酸盐岩储层特征及主控因素——以塔里木盆地阿克苏地区下寒武统肖尔布拉克组上段为例
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摘要
通过野外露头观察,室内薄片鉴定以及物性分析,详细分析了塔里木盆地阿克苏地区下寒武统肖尔布拉克组上段微生物碳酸盐岩储层特征及其主控因素。研究认为肖上段主要发育微生物礁和微生物层这两种巨观构造,其中前者包括凝块石礁和表附菌礁,后者包括凝块石层、表附菌层、叠层石层、层纹石层和泡沫绵层。微生物碳酸盐岩具有多种与微生物相关的孔隙,同时也具有非微生物储集空间。凝块石礁和泡沫绵层是最有利的微生物储层,表明不同类型的微生物岩储层具有较大的物性差别。于提希剖面和苏盖特布拉克剖面对比发现,相同类型的微生物岩储层亦具有较大的差异,这是因为微生物碳酸盐岩储层的形成与保存受控于沉积相分布、古地貌特征、成岩作用以及微生物结构的缘故。
Through observation of field outcrops, identification of thin section and physical property analysis, the characteristics and main controlling factors of microbial carbonate reservoir in the upper member of Lower Cambrian Xiaoerbulake Formation in Akesu area, Tarim Basin have been examined in detail. It is concluded through the study that two kinds of megascopic structures are developed, including microbial reef and microbial layer in this member; the former includes thrombolite reef and Epiphyton reef, and the later contains thrombolite, Epiphyton, stromatolite, laminite and spongiostromata biostromes. The microbial carbonate contains a variety of pores related to microbes and also non-microbial reservoir space. Thrombolite reef and spongiostromata biostrome are the most favorable microbial reservoirs, indicating different types of microbialite reservoirs differ widely in physical properties. The comparison of Yutixi profile with Sugetbulak profile shows that even the same type of microbialite reservoirs differ considerably. This is because the formation and preservation of microbial carbonate reservoirs are affected by the distribution of sedimentary facies, ancient landform features, diageneses and microbial structures.
Through observation of field outcrops, identification of thin section and physical property analysis, the characteristics and main controlling factors of microbial carbonate reservoir in the upper member of Lower Cambrian Xiaoerbulake Formation in Akesu area, Tarim Basin have been examined in detail. It is concluded through the study that two kinds of megascopic structures are developed, including microbial reef and microbial layer in this member; the former includes thrombolite reef and Epiphyton reef, and the later contains thrombolite, Epiphyton, stromatolite, laminite and spongiostromata biostromes. The microbial carbonate contains a variety of pores related to microbes and also non-microbial reservoir space. Thrombolite reef and spongiostromata biostrome are the most favorable microbial reservoirs, indicating different types of microbialite reservoirs differ widely in physical properties. The comparison of Yutixi profile with Sugetbulak profile shows that even the same type of microbialite reservoirs differ considerably. This is because the formation and preservation of microbial carbonate reservoirs are affected by the distribution of sedimentary facies, ancient landform features, diageneses and microbial structures.
引文
[1]Burne R V,Moore L S.Microbialites:organosedimentary deposits of benthic microbial communities[J].Palaios,1987,2(3):241-254.
[2]Riding R.Classification of microbial carbonates[C]//Riding R.Calcareous Algae and Stromatolite.Berlin:Springer-Verlag,1991:21-51.
[3]Riding R.Microbial carbonates:the geological record of calcified bacterial-algal mats and biofilms[J].Sedimentology,2000,47(Supp.1):179-214.
[4]Riding R.Mircobial carbonate abundance compared with fluctuations in metazoan diversity over geological time[J].Sedimentary Geology,2006,185:229-238.
[5]Riding R.An atmospheric stimulus for cyanobacterialbioinduced calcification CA.350 Million years ago[J].Palaios,2009,24:685-696.
[6]Riding R.A hard life for Cyanobacteria[J].Science,2012,336:427-428.
[7]戴永定,陈孟莪,王尧.微生物岩研究的发展和展望[J].地球科学进展,1996,11(2):209-215.Dai Yongding,Chen Meng′e,Wang Yao.Development and perspective of research for microbolites[J].Advance in Earth Sciences,1996,11(2):209-215.
[8]梅冥相,孟庆芬,刘智荣.微生物形成的原生沉积构造研究进展综述[J].古地理学报,2007,9(4):353-367.Mei Mingxiang,Meng Qingfen,Liu Zhirong.Overview of advances in studies of primary sedimentary structures formed by microbes[J].Journal of Palaeogeography,2007,9(4):353-367.
[9]梅冥相.微生物碳酸盐岩分类体系的修订:对灰岩成因结构分类体系的补充[J].地学前缘,2007,14(5):222-234.Mei Mingxiang.Revised classification of microbial carbonates:complementing the classification of limestones[J].Earth Science Frontiers,2007,14(5):222-234.
[10]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.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.
[11]韩作振,陈吉涛,迟乃杰,王兆鹏,杨仁超,樊爱萍.微生物碳酸盐岩研究:回顾与展望[J].海洋地质与第四纪地质.2009,29(4):30-38.Han Zuozhen,Chen Jitao,Chi Naijie,Wang Zhaopeng,Yang Renchao,Fan Aiping.Microbial carbonates:a review and perspectives[J].Marine geology&quaternary geology,2009,29(4):30-38.
[12]韩作振,陈吉涛,张晓蕾,于学峰.鲁西寒武系第三统张夏组附枝菌与附枝菌微生物灰岩特征研究[J].地质学报,2009,83(8):1097-1103.Han Zuozhen,Chen Jitao,Zhang Xiaolei,Yu Xuefeng.Characteristics of epiphyton and epiphyton microbialites in the Zhangxia Formation(Third Series of Cambrian),Shandong Province[J].Acta Geologica Sinica,2009,83(8):1097-1103.
[13]罗平,王石,李朋威,宋金民,金廷福,王果谦,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.Luo Ping,Wang Shi,Li Pengwei,Song Jinmin,Jin Tingfu,Wang Guoqian,et al.Review and prospectives of microbial carbonate reservoirs[J].Acta Sedimentology Sinica,2013,31(5):807-823.
[14]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):1163-1178.
[15]Awramik S M.Stromatolite Newsletter[J].Lethaia,1977,10(1):42-42.
[16]Whitton B A.The ecology of cyanobacteria:their diversity in time and space[C]//Whitton B A,Potts M.The ecology of cyanobacteria:their diversity in time and space.Dordrecht:Kluwer Academic Publishers,2000:233-255.
[17]Herrero A,Flores E.The cyanobacteria:molecular biology,genomics and evolution[M].Spain:Caister Academic Press,2008.
[18]Kennard J M,James N P.Thrombolites and stromatolites;two distinct types of microbial structures[J].Palaios,1986,1:492-503.
[19]Leinfelder R R,Schmid D U.Mesozoic reefal thrombolites and other microbolites[C]//Riding R.Microbial sediments.Berlin:Springer,2010:289-294.
[20]刘乃震,王国勇,熊小林.地质工程一体化技术在威远页岩气高效开发中的实践与展望[J].中国石油勘探,2018,23(2):59-68.Liu Naizhen,Wang Guoyong,Xiong Xiaolin.Practice and prospect of geology-engineering integration technology in the efficient development of shale gas in Weiyuan block.China Petroleum Exploration,2018,23(2):59-68.
[21]游靖,徐建昌,余吉良,孙霜青,李春玲,胡松青.华北宝力格油田水处理系统微生物群落结构及多样性分析[J].油气地质与采收率,2016,23(5):76-82.You Jing,Xu Jianchang,Yu Jiliang,Sun Shuangqing,Li Chunling,Hu Songqing.Analysis of microbial community structure and diversity of the water treatment system in Huabei Baolige oilfield[J].Petroleum Geology and Recovery Efficiency,2016,23(5):76-82.
[22]Shapiro R S.A comment on the systematic confusion of thrombolites[J].Palaios,2000,15:166-169.
[23]宋金民.塔里木盆地寒武系白云岩储层类型、成因及分布规律[D].北京:中国石油勘探开发研究院,2012.Song Jinmin.Types,genesis,and distribution of dolomite reservoirs,Cambrian,Tarim Basin[D].Beijing:Petro China Research Institute of Petroleum Exploration&Development,2012.
[24]宋金民,罗平,杨式升,翟秀,周刚,陆朋朋.塔里木盆地苏盖特布拉克地区下寒武统肖尔布拉克组碳酸盐岩微生物建造特征[J].古地理学报,2012,14(3):341-254.Song Jinmin,Luo Ping,Yang Shisheng,Zhai Xiufen,Zhou Gang,Lu Pengpeng.Carbonate rock microbial construction of the Lower Cambrian Xiaoerblak Formation in Sugaitblak area,Tarim Basin[J].Journal of Palaeogeography,2012,14(3):341-254.
[25]宋金民,罗平,杨式升,杨迪,周川闽,李朋威,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.Song Jinmin,Luo Ping,Yang Shisheng,Yang Di,Zhou Chuanmin,Li Pengwei,et al.Reservoirs of Lower Cambrian microbial carbonates,Tarim Basin,NW China[J].Petroleum Exploration and Development,2014,41(4):404-413.
[26]王石.塔里木盆地寒武系微生物岩储层结构和分布[D].北京:中国石油勘探开发研究院,2014.Wang Shi.Structure and distribution of microbial carbonate reservoirs,Cambrian,Tarim Basin[D].Beijing:Petro China Research Institute of Petroleum Exploration&Development,2014.
[27]谢会文,能源,敬兵,朱永峰,王斌.塔里木盆地寒武系—奥陶系白云岩潜山勘探新发现与勘探意义[J].中国石油勘探,2017,22(3):1-11.Xie Huiwen,Neng Yuan,Jing Bing,Zhu Yongfeng,Wang Bin.New discovery in exploration of Cambrian-Ordovician dolomite buried hills in Tarim Basin and its significance[J].China Petroleum Exploration,2017,22(3):1-11.
[28]赵宗举,罗家洪,张运波,吴兴宁,潘文庆.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.Zhao Zongju,Luo Jiahong,Zhang Yunbo,Wu Xingning,Pan Wenqing.Lithofacies paleogeography of Cambrian sequences in the Tarim Basin[J].Acta Petrolei Sinica,2011,32(6):937-948.
[29]贾承造,张师本,吴绍祖.塔里木盆地及周边地层[M].北京:科学出版社,2004.Jia Chengzao,Zhang Shiben,Wu Shaozu.Stratigraphy of the Tarim Basin and adjacent areas[M].Beijing:Science Press,2004.
[30]冯增昭,彭勇民,金振奎,鲍志东.中国早寒武世岩相古地理[J].古地理学报,2002,4(1):1-12.Feng Zengzhao,Peng Yongmin,Jin Zhenkui,Bao Zhidong.Lithofacies palaeogeography of the early Cambrian in China[J].Journal of Palaeogeography,2002,4(1):1-12.
[31]冯增昭,鲍志东,吴茂炳,金振奎,时晓章.塔里木地区寒武纪和奥陶纪岩相古地理[M].北京:地质出版社,2005.Feng Zengzhao,Bao Zhidong,Wu Maobing,Jin Zhenkui,Shi Xiaozhang.Lithofacies palaeogeography of the Cambrian and Ordovician in Tarim area[M].Beijing:Geological Publishing House,2005.
[32]冯增昭,鲍志东,吴茂炳,金振奎,时晓章,塔里木地区寒武纪岩相古地理[J].古地理学报,2006,8(4):427-439.Feng Zengzhao,Bao Zhidong,Wu Maobing,Jin Zhenkui,Shi Xiaozhang.Lithofacies palaeogeography of the Cambrian in Tarim area[J].Journal of Palaeogeography,2006,8(4):427-439.
[33]Paterson D M.Microbiological mediation of sediment structure and behavior[C]//Stal L J,Caumette P.Microbial mats.Berlin:Springer-Verlag,1994:97-109.
[34]Noffke N,Gerdes G,Klenke T.Benthic cyanobacteria and their influence on the sedimentary dynamics of peritidal system(Siliclastic,evaporitic salty,and evaporitic carbonatic)[J].Earth-Science Reviews,2003,62:163-176.
[35]Pratt B R.Epiphyton and renalcis-diagenetic microfossils from calcification of coccoid blue-green algae[J].AAPG Bulletin,1984,54(3):948-971.
[36]彭瀚霖,刘树根,宋金民,孙玮,丁一,尹柯惟.川北米仓山地区灯影组微生物碳酸盐岩发育特征[J].成都理工大学学报:自然科学版,2014,41(2):181-191.Peng Hanlin,Liu Shugen,Song Jinmin,Sun Wei,Ding Yi,Yin Kewei.Characteristics of microbial carbonate rocks in Upper Sinian Dengying Formation of Micang Mountains,north Sichuan,China[J].Journal of Chengdu University of Technology:Science&Technology Edition,2014,41(2):181-191.
[37]Woo J,Chough S K,Han Z.Chambers of epiphyton thalli in microbial buildups,Zhangxia Formation(Middle Cambrian),Shandong Province,China[J].Palaios,2008,22:55-64.
[38]李朋威,罗平,陈敏,宋金民,金廷福,王果谦.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.Li Pengwei,Luo Ping,Chen Min,Song Jinmin,Jin Tingfu,Wang Guoqian.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.
[39]李朋威,罗平,宋金民,金廷福,王果谦.微生物碳酸盐岩储层特征与主控因素——以塔里木盆地西北缘上震旦统—下寒武统为例[J].石油学报,2015,36(9):1074-1089.Li Pengwei,Luo Ping,Song Jinmin,Jin Tingfu,Wang Guoqian.Characteristics and main controlling factors of microbial carbonate reservoirs:a case study of Upper SinianLower Cambrian in the northwestern margin of Tarim Basin[J].Acta Petrolei Sinica,2015,36(9):1074-1089.
[40]张荫本,唐泽尧,陈季高.粘结岩分类及应用[J].天然气勘探与开发,1996(4):194-198.Zhang Yinben,Tang Zeyao,Chen Jigao.Classification and application of the boundstone[J].Natural Gas Exploration and Development,1996(4):194-198.
[41]黄思静.碳酸盐岩的成岩作用[M].北京:地质出版社,2010.Huang Sijing.Carbonate diagenesis[M].Beijing:Geological Publishing House,2010.
[42]王凯,关平,邓世彪,刘沛显,金亦秋.塔里木盆地下寒武统微生物礁储集性研究及油气勘探意义[J].沉积学报,2016,34(2):386-396.Wang Kai,Guan Ping,Deng Shibiao,Liu Peixian,Jin Yiqiu.Reservoirs of the Lower Cambrian microbial reefs and its significance on petroleum exploration,Tarim Basin,NW China[J].Acta Sedimentologica Sinica,2016,34(2):386-396.
[43]张静,胡见义,罗平,宋金民.深埋优质白云岩储集层发育的主控因素与勘探意义[J].石油勘探与开发,2010,37(2):203-210.Zhang Jing,Hu Jianyi,Luo Ping,Song Jinmin.Master control factors of deep high-quality dolomite reservoirs and the exploration significance[J].Petroleum Exploration and Development,2010,37(2):203-210.
[44]胡明毅.塔里木盆地北部寒武系碳酸盐岩成岩作用及孔隙演化[J].江汉石油学院学报,1993,15(2):1-8.Hu Mingyi.Diagenesis and porosity evolution of Cambrian carbonate rock,in the north Tarim Basin[J].Journal of Jianghan Petroleum Institute,1993,15(2):1-8.
[2]Riding R.Classification of microbial carbonates[C]//Riding R.Calcareous Algae and Stromatolite.Berlin:Springer-Verlag,1991:21-51.
[3]Riding R.Microbial carbonates:the geological record of calcified bacterial-algal mats and biofilms[J].Sedimentology,2000,47(Supp.1):179-214.
[4]Riding R.Mircobial carbonate abundance compared with fluctuations in metazoan diversity over geological time[J].Sedimentary Geology,2006,185:229-238.
[5]Riding R.An atmospheric stimulus for cyanobacterialbioinduced calcification CA.350 Million years ago[J].Palaios,2009,24:685-696.
[6]Riding R.A hard life for Cyanobacteria[J].Science,2012,336:427-428.
[7]戴永定,陈孟莪,王尧.微生物岩研究的发展和展望[J].地球科学进展,1996,11(2):209-215.Dai Yongding,Chen Meng′e,Wang Yao.Development and perspective of research for microbolites[J].Advance in Earth Sciences,1996,11(2):209-215.
[8]梅冥相,孟庆芬,刘智荣.微生物形成的原生沉积构造研究进展综述[J].古地理学报,2007,9(4):353-367.Mei Mingxiang,Meng Qingfen,Liu Zhirong.Overview of advances in studies of primary sedimentary structures formed by microbes[J].Journal of Palaeogeography,2007,9(4):353-367.
[9]梅冥相.微生物碳酸盐岩分类体系的修订:对灰岩成因结构分类体系的补充[J].地学前缘,2007,14(5):222-234.Mei Mingxiang.Revised classification of microbial carbonates:complementing the classification of limestones[J].Earth Science Frontiers,2007,14(5):222-234.
[10]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.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.
[11]韩作振,陈吉涛,迟乃杰,王兆鹏,杨仁超,樊爱萍.微生物碳酸盐岩研究:回顾与展望[J].海洋地质与第四纪地质.2009,29(4):30-38.Han Zuozhen,Chen Jitao,Chi Naijie,Wang Zhaopeng,Yang Renchao,Fan Aiping.Microbial carbonates:a review and perspectives[J].Marine geology&quaternary geology,2009,29(4):30-38.
[12]韩作振,陈吉涛,张晓蕾,于学峰.鲁西寒武系第三统张夏组附枝菌与附枝菌微生物灰岩特征研究[J].地质学报,2009,83(8):1097-1103.Han Zuozhen,Chen Jitao,Zhang Xiaolei,Yu Xuefeng.Characteristics of epiphyton and epiphyton microbialites in the Zhangxia Formation(Third Series of Cambrian),Shandong Province[J].Acta Geologica Sinica,2009,83(8):1097-1103.
[13]罗平,王石,李朋威,宋金民,金廷福,王果谦,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.Luo Ping,Wang Shi,Li Pengwei,Song Jinmin,Jin Tingfu,Wang Guoqian,et al.Review and prospectives of microbial carbonate reservoirs[J].Acta Sedimentology Sinica,2013,31(5):807-823.
[14]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):1163-1178.
[15]Awramik S M.Stromatolite Newsletter[J].Lethaia,1977,10(1):42-42.
[16]Whitton B A.The ecology of cyanobacteria:their diversity in time and space[C]//Whitton B A,Potts M.The ecology of cyanobacteria:their diversity in time and space.Dordrecht:Kluwer Academic Publishers,2000:233-255.
[17]Herrero A,Flores E.The cyanobacteria:molecular biology,genomics and evolution[M].Spain:Caister Academic Press,2008.
[18]Kennard J M,James N P.Thrombolites and stromatolites;two distinct types of microbial structures[J].Palaios,1986,1:492-503.
[19]Leinfelder R R,Schmid D U.Mesozoic reefal thrombolites and other microbolites[C]//Riding R.Microbial sediments.Berlin:Springer,2010:289-294.
[20]刘乃震,王国勇,熊小林.地质工程一体化技术在威远页岩气高效开发中的实践与展望[J].中国石油勘探,2018,23(2):59-68.Liu Naizhen,Wang Guoyong,Xiong Xiaolin.Practice and prospect of geology-engineering integration technology in the efficient development of shale gas in Weiyuan block.China Petroleum Exploration,2018,23(2):59-68.
[21]游靖,徐建昌,余吉良,孙霜青,李春玲,胡松青.华北宝力格油田水处理系统微生物群落结构及多样性分析[J].油气地质与采收率,2016,23(5):76-82.You Jing,Xu Jianchang,Yu Jiliang,Sun Shuangqing,Li Chunling,Hu Songqing.Analysis of microbial community structure and diversity of the water treatment system in Huabei Baolige oilfield[J].Petroleum Geology and Recovery Efficiency,2016,23(5):76-82.
[22]Shapiro R S.A comment on the systematic confusion of thrombolites[J].Palaios,2000,15:166-169.
[23]宋金民.塔里木盆地寒武系白云岩储层类型、成因及分布规律[D].北京:中国石油勘探开发研究院,2012.Song Jinmin.Types,genesis,and distribution of dolomite reservoirs,Cambrian,Tarim Basin[D].Beijing:Petro China Research Institute of Petroleum Exploration&Development,2012.
[24]宋金民,罗平,杨式升,翟秀,周刚,陆朋朋.塔里木盆地苏盖特布拉克地区下寒武统肖尔布拉克组碳酸盐岩微生物建造特征[J].古地理学报,2012,14(3):341-254.Song Jinmin,Luo Ping,Yang Shisheng,Zhai Xiufen,Zhou Gang,Lu Pengpeng.Carbonate rock microbial construction of the Lower Cambrian Xiaoerblak Formation in Sugaitblak area,Tarim Basin[J].Journal of Palaeogeography,2012,14(3):341-254.
[25]宋金民,罗平,杨式升,杨迪,周川闽,李朋威,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.Song Jinmin,Luo Ping,Yang Shisheng,Yang Di,Zhou Chuanmin,Li Pengwei,et al.Reservoirs of Lower Cambrian microbial carbonates,Tarim Basin,NW China[J].Petroleum Exploration and Development,2014,41(4):404-413.
[26]王石.塔里木盆地寒武系微生物岩储层结构和分布[D].北京:中国石油勘探开发研究院,2014.Wang Shi.Structure and distribution of microbial carbonate reservoirs,Cambrian,Tarim Basin[D].Beijing:Petro China Research Institute of Petroleum Exploration&Development,2014.
[27]谢会文,能源,敬兵,朱永峰,王斌.塔里木盆地寒武系—奥陶系白云岩潜山勘探新发现与勘探意义[J].中国石油勘探,2017,22(3):1-11.Xie Huiwen,Neng Yuan,Jing Bing,Zhu Yongfeng,Wang Bin.New discovery in exploration of Cambrian-Ordovician dolomite buried hills in Tarim Basin and its significance[J].China Petroleum Exploration,2017,22(3):1-11.
[28]赵宗举,罗家洪,张运波,吴兴宁,潘文庆.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.Zhao Zongju,Luo Jiahong,Zhang Yunbo,Wu Xingning,Pan Wenqing.Lithofacies paleogeography of Cambrian sequences in the Tarim Basin[J].Acta Petrolei Sinica,2011,32(6):937-948.
[29]贾承造,张师本,吴绍祖.塔里木盆地及周边地层[M].北京:科学出版社,2004.Jia Chengzao,Zhang Shiben,Wu Shaozu.Stratigraphy of the Tarim Basin and adjacent areas[M].Beijing:Science Press,2004.
[30]冯增昭,彭勇民,金振奎,鲍志东.中国早寒武世岩相古地理[J].古地理学报,2002,4(1):1-12.Feng Zengzhao,Peng Yongmin,Jin Zhenkui,Bao Zhidong.Lithofacies palaeogeography of the early Cambrian in China[J].Journal of Palaeogeography,2002,4(1):1-12.
[31]冯增昭,鲍志东,吴茂炳,金振奎,时晓章.塔里木地区寒武纪和奥陶纪岩相古地理[M].北京:地质出版社,2005.Feng Zengzhao,Bao Zhidong,Wu Maobing,Jin Zhenkui,Shi Xiaozhang.Lithofacies palaeogeography of the Cambrian and Ordovician in Tarim area[M].Beijing:Geological Publishing House,2005.
[32]冯增昭,鲍志东,吴茂炳,金振奎,时晓章,塔里木地区寒武纪岩相古地理[J].古地理学报,2006,8(4):427-439.Feng Zengzhao,Bao Zhidong,Wu Maobing,Jin Zhenkui,Shi Xiaozhang.Lithofacies palaeogeography of the Cambrian in Tarim area[J].Journal of Palaeogeography,2006,8(4):427-439.
[33]Paterson D M.Microbiological mediation of sediment structure and behavior[C]//Stal L J,Caumette P.Microbial mats.Berlin:Springer-Verlag,1994:97-109.
[34]Noffke N,Gerdes G,Klenke T.Benthic cyanobacteria and their influence on the sedimentary dynamics of peritidal system(Siliclastic,evaporitic salty,and evaporitic carbonatic)[J].Earth-Science Reviews,2003,62:163-176.
[35]Pratt B R.Epiphyton and renalcis-diagenetic microfossils from calcification of coccoid blue-green algae[J].AAPG Bulletin,1984,54(3):948-971.
[36]彭瀚霖,刘树根,宋金民,孙玮,丁一,尹柯惟.川北米仓山地区灯影组微生物碳酸盐岩发育特征[J].成都理工大学学报:自然科学版,2014,41(2):181-191.Peng Hanlin,Liu Shugen,Song Jinmin,Sun Wei,Ding Yi,Yin Kewei.Characteristics of microbial carbonate rocks in Upper Sinian Dengying Formation of Micang Mountains,north Sichuan,China[J].Journal of Chengdu University of Technology:Science&Technology Edition,2014,41(2):181-191.
[37]Woo J,Chough S K,Han Z.Chambers of epiphyton thalli in microbial buildups,Zhangxia Formation(Middle Cambrian),Shandong Province,China[J].Palaios,2008,22:55-64.
[38]李朋威,罗平,陈敏,宋金民,金廷福,王果谦.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.Li Pengwei,Luo Ping,Chen Min,Song Jinmin,Jin Tingfu,Wang Guoqian.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.
[39]李朋威,罗平,宋金民,金廷福,王果谦.微生物碳酸盐岩储层特征与主控因素——以塔里木盆地西北缘上震旦统—下寒武统为例[J].石油学报,2015,36(9):1074-1089.Li Pengwei,Luo Ping,Song Jinmin,Jin Tingfu,Wang Guoqian.Characteristics and main controlling factors of microbial carbonate reservoirs:a case study of Upper SinianLower Cambrian in the northwestern margin of Tarim Basin[J].Acta Petrolei Sinica,2015,36(9):1074-1089.
[40]张荫本,唐泽尧,陈季高.粘结岩分类及应用[J].天然气勘探与开发,1996(4):194-198.Zhang Yinben,Tang Zeyao,Chen Jigao.Classification and application of the boundstone[J].Natural Gas Exploration and Development,1996(4):194-198.
[41]黄思静.碳酸盐岩的成岩作用[M].北京:地质出版社,2010.Huang Sijing.Carbonate diagenesis[M].Beijing:Geological Publishing House,2010.
[42]王凯,关平,邓世彪,刘沛显,金亦秋.塔里木盆地下寒武统微生物礁储集性研究及油气勘探意义[J].沉积学报,2016,34(2):386-396.Wang Kai,Guan Ping,Deng Shibiao,Liu Peixian,Jin Yiqiu.Reservoirs of the Lower Cambrian microbial reefs and its significance on petroleum exploration,Tarim Basin,NW China[J].Acta Sedimentologica Sinica,2016,34(2):386-396.
[43]张静,胡见义,罗平,宋金民.深埋优质白云岩储集层发育的主控因素与勘探意义[J].石油勘探与开发,2010,37(2):203-210.Zhang Jing,Hu Jianyi,Luo Ping,Song Jinmin.Master control factors of deep high-quality dolomite reservoirs and the exploration significance[J].Petroleum Exploration and Development,2010,37(2):203-210.
[44]胡明毅.塔里木盆地北部寒武系碳酸盐岩成岩作用及孔隙演化[J].江汉石油学院学报,1993,15(2):1-8.Hu Mingyi.Diagenesis and porosity evolution of Cambrian carbonate rock,in the north Tarim Basin[J].Journal of Jianghan Petroleum Institute,1993,15(2):1-8.