海相优质页岩的形成环境及发育模式——以中扬子地区秭归新滩剖面五峰—龙马溪组页岩为例
|
摘要
运用地球化学和岩石学方法,从古盐度、古气候、古生产力、海域封闭性以及氧化还原条件等方面,分析中扬子地区秭归新滩剖面上奥陶统五峰组—下志留统龙马溪组海相优质页岩的形成环境,并探讨了优质页岩发育的控制因素及模式。结果表明:中扬子地区五峰—龙马溪组优质页岩以硅质页岩为主,主要发育在五峰组至埃隆阶底部;优质页岩主要形成于温暖潮湿、低盐度—正常盐度、弱封闭—半封闭的缺氧环境中,并且具有较高的古生产力;海相优质页岩的发育是构造活动、海平面升降以及陆源—生物硅质供应等多因素综合作用的结果,而在埃隆期之后,随着扬子板块的持续向西北推进,海域面积不断萎缩,生物硅质供应降低,陆源碎屑供应迅速增加,优质页岩不再发育。最后,总结了海相优质页岩的发育模式。
This paper analyzes the forming environment of high-quality marine shale in the Ordovician Wufeng Formation and the Lower Silurian Longmaxi Formation in the Zigui-Xitan section in the MiddleYangtze region from the aspects of paleo-salinity,palaeoclimate,paleo-productivity,sea area closure and REDOX conditions by using geochemical and petrologic methods,and discusses the controlling factors and development model of high-quality marine shale. The results show that: The high-quality shale of the Wufeng-Longmaxi Formations in the Middle Yangtze region is mainly siliceous shale,which is mainly developed from the Wufeng Formation to the bottom of Aeronian; High-quality shale is mainly formed in the anoxic environment with warm and humid palaeoclimate,low salinity to normal salinity and weakly enclosed to semi-enclosed conditions,and it has a high paleo-productivity. The development of marine highquality shale is a comprehensive result of multiple factors including tectonic activities,sea-level change and terrigenous-biological siliceous supply,and After Aeronian,the Yangtze plate continuously moved northwestward and sea area reduced,causing a rapid decrease of autogenous siliceous materials and increase of terrigenous clasts. Consequently,high-quality marine shale no longer existed. Finally,the development model of high-quality marine shale is summarized.
This paper analyzes the forming environment of high-quality marine shale in the Ordovician Wufeng Formation and the Lower Silurian Longmaxi Formation in the Zigui-Xitan section in the MiddleYangtze region from the aspects of paleo-salinity,palaeoclimate,paleo-productivity,sea area closure and REDOX conditions by using geochemical and petrologic methods,and discusses the controlling factors and development model of high-quality marine shale. The results show that: The high-quality shale of the Wufeng-Longmaxi Formations in the Middle Yangtze region is mainly siliceous shale,which is mainly developed from the Wufeng Formation to the bottom of Aeronian; High-quality shale is mainly formed in the anoxic environment with warm and humid palaeoclimate,low salinity to normal salinity and weakly enclosed to semi-enclosed conditions,and it has a high paleo-productivity. The development of marine highquality shale is a comprehensive result of multiple factors including tectonic activities,sea-level change and terrigenous-biological siliceous supply,and After Aeronian,the Yangtze plate continuously moved northwestward and sea area reduced,causing a rapid decrease of autogenous siliceous materials and increase of terrigenous clasts. Consequently,high-quality marine shale no longer existed. Finally,the development model of high-quality marine shale is summarized.
引文
常华进,储雪蕾,冯连君,黄晶,张启锐.2009.氧化还原敏感微量元素对古海洋沉积环境的指示意义.地质论评,55(1):91-99.[Chang H J,Chu X L,Feng L J,Huang J,Zhang Q R.2009.Redox sensitive trace element as Paleoenvironments Proxies.Geological review,55(1):91-99]
陈孝红,张保民,陈林,张国涛,李培军,张淼.2018.鄂西宜昌地区晚奥陶世-早志留世页岩气藏的主控地质因素与富集模式.地球学报,39(3):257-268.[Chen X H,Zhang B M,Chen L,Zhang G T,Li P J,Zhang M.2018.Main geological controlling factors and enrichment pattern of shale gas reservoirs in the Late OrdovicianEarly Silurian Strata of Yichang,Western Hubei Province.Acta Geoscientica Sinica,39(3):257-268]
陈旭,戎嘉余,周志毅,张元动,詹仁斌,刘建波,樊隽轩.2001.上扬子区奥陶-志留纪之交的黔中隆起和宜昌上升.科学通报,46(12):1052-1056.[Chen X,Rong J Y,Zhou Z Y,Zhang Y D,Zhan R B,Liu J B,Fan J X.2001.Qianzhong upheaval and Yichang rise formed at transition between the Ordovician and Silurian in Upper Yangtze Region.Chinese Science Bulletin,46(12):1052-1056]
陈旭,樊隽轩,王文卉,王红岩,聂海宽,石学文,文治东,陈冬阳,李文杰.2017.黔渝地区志留系龙马溪组黑色笔石页岩的阶段性渐进展布模式.中国科学:地球科学,47(6):720-732.[Chen X,Fan J X,Wang W H,Wang H Y,Nie H K,Shi X W,Wen Z D,Chen D Y,Li W J.2017.Stage-progressive distribution pattern of the Lungmachi black graptolitic shales from Guizhou to Chongqing,Central China.Science China Earth Science,47(6):720-732]
戴少武.2002.中扬子及邻区层序地层与原型盆地演化.石油与天然气地质,23(3):229-235.[Dai S W.2002.Stratigraphy sequences in the Middle Yangtze&adjacent region and evolution of prototype basins.Oil&Gas Geology,23(3):229-235]
樊隽轩,Melchin M J,陈旭,王怿,张元动,陈清,迟昭利,陈峰.2012.华南奥陶-志留系龙马溪组黑色笔石页岩的生物地层学.中国科学(地球科学),42(1):130-139.[Fan J X,Melchin M J,Chen X,Wang Y,Zhang Y D,Chen Q,Chi Z L,Chen F.2012.Biostratigraphy and geography of the Ordovician-Silurian Lungmachi black shales in South China.Scientia Sinica Terrae,42(1):130-139]
冯洪真,Erdtmann B D,王海峰.2000.上扬子区早古生代全岩Ce异常与海平面长缓变化.中国科学(D辑),30(1):66-72.[Feng H Z,Erdtmann B D,Wang H F.2000.Early Paleozoic whole-rock Ce anomalies and secular eustatic changes in the Upper Yangtze region.Science in China(Series D),30(1):66-72]
郭旭升,梅廉夫,汤济广,沈传波.2006.扬子地块中新生代构造演化对海相油气成藏的制约.石油与天然气地质,27(3):295-325.[Guo X S,Mei L F,Tang J G,Shen C B.2006.Constraint of MesoCenozonic tectonic evolution of Yangtze massif on formation of marine reseroirs.Oil&Gas Geology,27(3):295-325]
郭旭升.2014.南方海相页岩气“二元富集”规律:四川盆地及周缘龙马溪组页岩气勘探实践认识.地质学报,88(7):1209-1218.[Guo X S.2014.Rules of Two-Factor Enrichiment for marine shale gas in Southern China:Understanding from the Longmaxi Formation shale gas in Sichuan Basin and its surrounding area.Acta Geologica Sinica,88(7):1209-1218]
郭旭升,胡东风,魏志红,李宇平,魏祥峰.2016.涪陵页岩气田的发现与勘探认识.中国石油勘探,21(3):24-37.[Guo X S,Hu DF,Wei Z H,Li Y P,Wei X F.2016.Discovery and exploration of Fuling Shale Gas Field.China Petroleum Exploration,21(3):24-37]
何卫红,汪啸风,卜建军.2003.扬子海盆中部晚奥陶世五峰期海平面变化.地球学报,24(1):55-60.[He W H,Wang X F,Bu J J.2003.Sea-level change of the central Yangtze Sea Basin in the Late Ordovician Wufengian Period.Acta Geoscientica Sinica,24(1):55-60]
焦方正,冯建辉,易积正,蔡勋育,何发岐.2015.中扬子地区海相天然气勘探方向、关键问题与勘探对策.中国石油勘探,20(2):1-8.[Jiao F Z,Feng J H,Yi J Z,Cai X Y,He F Q.2015.Direction,key factors and solution of marine natural gas exploration in Yangtze Area.China Petroleum Exploration,20(2):1-8]
李双建,肖开华,沃玉进,龙胜祥,蔡立国.2008.南方海相上奥陶统-下志留统优质烃源岩发育的控制因素.沉积学报,26(5):872-880.[Li S J,Xiao K H,Wo Y J,Long S X,Cai L G.2008.Development controlling factors of Upper Ordovician-Lower Silurian high quality source rocks in marine sequence,South China.Acta Sedimentologica Sinica,26(5):872-880]
梁狄刚,郭彤楼,陈建平,边立曾,赵喆.2009a.中国南方海相生烃成藏研究的若干新进展(二):南方四套区域性海相烃源岩的地球化学特征.海相油气地质,14(1):1-15.[Liang D G,Guo T L,Chen J P,Bian L Z,Zhao Z.2009a.Some progresses on studies of hydrocarbon generation and accumulation in marine sedimentary regions,Southern China(Part 2):Geochemical characteristics of four suits of regional marine source rocks,South China.Marine Origin Petroleum Geology,14(1):1-15]
梁狄刚,郭彤楼,边立曾,陈建平,赵喆.2009b.中国南方海相生烃成藏研究的若干新进展(三):南方四套区域性海相烃源岩的沉积相及发育的控制因素.海相油气地质,14(2):1-19.[Liang DG,Guo T L,Bian L Z,Chen J P,Zhao Z.2009b.Some progresses on studies of hydrocarbon generation and accumulation in marine sedimentary regions,southern China(Part 3):Controlling factors on the sedimentary facies and development of Palaeozoic marine souce rocks.Marine Origin Petroleum Geology,14(2):1-19]
梁峰,王红岩,拜文华,郭伟,赵群,孙莎莎,张琴,武瑾,马超,雷治安.2017.川南地区五峰组-龙马溪组页岩笔石带对比及沉积特征.天然气工业,37(7):20-26.[Liang F,Wang H Y,Bai W H,Guo W,Zhao Q,Sun S S,Zhang Q,Wu J,Ma Chao,Lei Z A.2017.Graptolite correlation and sedimentary characteristics of Wufeng-Longmaxi shale in southern Sichuan Basin.Natural Gas Industry,37(7):20-26]
牟传龙,葛祥英,许效松,周恳恳,梁薇,王秀平.2014.中上扬子地区晚奥陶世岩相古地理及其油气地质意义.古地理学报,16(4):427-440.[Mou C L,Ge X Y,Xu X S,Zhou K K,Liang W,Wang X P.2014.Lithofacies palaeogeography of the Late Ordovician and its petroleum geological significance in Middle-Upper Yangtze Region.Journal of Palaeogeography(Chinese Edition),16(4):427-440]
牟传龙,王秀平,王启宇,周恳恳,梁薇,葛祥英,陈小炜.2016.川南及邻区下志留统龙马溪组下段沉积相与页岩气地质条件的关系.古地理学报,18(3):457-472.[Mou C L,Wang X P,Wang Q Y,Zhou K K,Liang W,Ge X Y,Chen X W.2016.Relationship between sedimentary facies and shale gas geological conditions of the Lower Silurian Longmaxi Formation in southern Sichuan Basin and its adjacent areas.Journal of Palaeogeography(Chinese Edition),18(3):457-472]
聂海宽,金之钧,马鑫,刘忠宝,林拓,杨振恒.2017.四川盆地及邻区上奥陶统五峰组-下志留统龙马溪组底部笔石带及沉积特征.石油学报,38(2):160-174.[Nie H K,Jin Z J,Ma X,Liu Z B,Lin T,Yang Z H.2017.Graptolites zone and sedimentary characteristics of Upper Ordovician Wufeng Formation-Lower Silurian Longmaxi Formation in Sichuan Basin and its adjacent areas.Acta Petrolei Sinica,38(2):160-174]
邱晓松,杨波,胡明毅.2013.中扬子地区五峰组-龙马溪组页岩气储层及含气性特征.天然气地球科学,24(6):1274-1283.[Qiu X S,Yang B,Hu M Y.2013.Characteristics of shale reservoirs and gas content of Wufeng-Longmaxi Formation in the middle Yangtze region.Natural Gas Geoscience,24(6):1274-1283]
苏文博,李志明,史晓颖,周洪瑞,黄思骥,刘晓茗,陈晓雨,张继恩,杨红梅,贾柳静,Huff W D,Elttensohn F R.2006.华南五峰组-龙马溪组与华北下马岭组的钾质斑脱岩及黑色岩系:两个地史转折期板块构造运动的沉积响应.地学前缘,13(6):82-95.[Su W B,Li Z M,Shi X Y,Zhou H R,Huang S J,Liu X M,Chen X Y,Zhang J E,Yang H M,Jia L J,Huff W D,Elttensohn F R.2006.K-bentonites and black shales from the Wufeng-Longmaxi Formations(Early Paleozoic,South China)and Xiamaling Formation(Early Neoproterozoic,North China):Implications for tectonic processes during two important transitions.Earth Science Frontiers,13(6):82-95]
孙小勇,牟传龙,葛祥英,王远翀,门欣.2016.四川广元-陕西镇巴地区上奥陶统五峰组地球化学特征及沉积环境意义.沉积与特提斯地质,36(1):46-54.[Sun X Y,Mou C L,Ge X Y,Wang YC,M X.2016.Geochemistry and sedimentary environments of the Upper Ordovician Wufeng Formation in Guangyuan,northern Sichuan and Zhenba,southern Shanxi.Sedimentary Geology and Tethyan Geology,36(1):46-54]
腾格尔,刘文汇,徐永昌.2005.海相地层无机参数与烃源岩发育环境的相关研究:以鄂尔多斯盆地为例.石油与天然气地质,26(4):411-421.[Tenger,Liu W H,Xu Y C.2005.Study on relation between inorganic parameters in marine deposits and developmental environment of hydrocarbon source rocks:Taking Ordos basin as an example.Oil&Gas Geology,26(4):411-421]
王清晨,严德天,李双建.2008.中国南方志留系底部优质烃源岩发育的构造-环境模式.地质学报,82(3):289-297.[Wang QC,Yan D T,Li S J.2008.Developmental controlling factors of Upper Ordovician-Lower Silurian high quality source rocks in marine sequence,South China.Acta Geologica Sinica,82(3):289-297]
王淑芳,邹才能,董大忠,王玉满,黄金亮,郭召杰.2014.四川盆地富有机质页岩硅质生物成因及对页岩气开发的意义.北京大学学报(自然科学版),50(3):476-486.[Wang S F,Zou C N,Dong D Z,Wang Y M,Huang J L,Guo Z J.2014.Biogenic silica of organic-rich shale in Sichuan Basin and its significance for shale gas.Acta Scientiarum Naturalium Universitatis Pekinensis,50(3):476-486]
王涛利,郝爱胜,陈清,李超,王庆涛,卢鸿,刘大永.2018.中扬子宜昌地区五峰组和龙马溪组页岩发育主控因素.天然气地球科学,29(5):616-631.[Wang T L,Hao A S,Chen Q,Li C,Wang Q T,Lu H,Liu D Y.2018.The study of main factors controlling the development of Wufeng Formation and Longmaxi Formation organicrich shales in the Yichang area,Middle Yangtze Region.Natural Gas Geoscience,29(5):616-631]
王怿,戎嘉余,詹仁斌,黄冰,吴荣昌,王光旭.2013.鄂西南奥陶系-志留系交界地层研究兼论宜昌上升.地层学杂志,37(3):264-274.[Wang Y,Rong J Y,Zhan R B,Huang B,Wu R C,Wang G X.2013.On the Ordovician-Silurian boundary strata in Southwest Hubei,and the Yichang Uplift.Journal of Stratigraphy,37(3):264-274]
王玉满,王淑芳,董大忠,李新景,黄金亮,张晨晨,管全中.2016.川南下志留统龙马溪组页岩岩相表征.地学前缘,23(1):119-133.[Wang Y M,Wang S F,Dong D Z,Li X J,Huang J L,Zhang CC,Guan Q Z.2016.Lithofacies characterization of Longmaxi Formation of the Lower Silurian,southern Sichuan.Earth Science Frontiers,23(1):119-133]
王玉满,李新景,董大忠,张晨晨,王淑芳.2017.上扬子地区五峰组-龙马溪组优质页岩沉积主控因素.天然气工业,37(4):9-20.[Wang Y M,Li X J,Dong D Z,Zhang C C,Wang S F.2017.Main factors controlling the sedimentation of high-quality shale in Wufeng-Longmaxi Fm,Upper Yangtze region.Natural Gas Industry,37(4):9-20]
王玉满,李新景,陈波,韩京,张家铭,袁飞,马杰,代兵,王浩,蒋珊.2018.中上扬子地区埃隆阶最厚斑脱岩层分布特征及地质意义.天然气地球科学,29(1):42-54.[Wang Y M,Li X J,Chen B,Han J,Zhang J M,Yuan F,Ma J,Dai B,Wang H,Jiang S.2018.Distribution characteristics and geological significance of the thickest Aeronian bentonite bed in Middle-Upper Yangtze Region.Natural Gas Geoscience,29(1):42-54]
王志刚.2015.涪陵页岩气勘探开发重大突破与启示.石油与天然气地质,36(1):1-6.[Wang Z G.2015.Breakthrough of Fuling shale gas exploration and development and its inspiration.Oil&Gas Geology,36(1):1-6]
吴蓝宇,陆永潮,蒋恕,刘晓峰,何贵松.2018.上扬子区奥陶系五峰组-志留系龙马溪组沉积期火山活动对页岩有机质富集程度的影响.石油勘探与开发,45(5):806-816.[Wu L Y,Lu Y C,Jiang S,Liu X F,He G S.2018.Effects of volcanic activities in Ordovician Wufeng-Silurian Longmaxi period on organic-rich shale in the Upper Yangtze area,South China.Petroleum Exploration and Development,45(5):806-816]
熊国庆,王剑,李园园,余谦,门玉澎,周小琳,熊小辉,周业鑫,杨潇.2017.大巴山地区早古生代黑色岩系岩相古地理及页岩气地质意义.古地理学报,19(6):965-986.[Xiong G Q,Wang J,Li Y Y,Yu Q,Men Y P,Zhou X L,Xiong X H,Zhou Y X,Yang X.2017.Lithofacies palaeogeography of the Early Paleozoic black rock series in Dabashan region and their shale-gas geological significance.Journal of Palaeogeography(Chinese Edition),19(6):965-986]
严德天,王清晨,陈代钊,汪建国,王卓卓.2008.扬子及周缘地区上奥陶统-下志留统烃源岩发育环境及其控制因素.地质学报,82(3):321-327.[Yan D T,Wang Q C,Chen D Z,Wang J G,Wang Z Z.2008.Sedimentary environment and development controls of the hydrocarbon sources beds:The Upper Ordovician Wufeng Formation and the Lower Silurian Longmaxi Formation in the Yangtze Area.Acta Geologica Sinica,82(3):321-327]
严德天,汪建国,王卓卓.2009.扬子地区上奥陶-下志留统生物钡特征及其古生产力意义.西安石油大学学报(自然科学版),24(4):16-19.[Yan D T,Wang J G,Wang Z Z.2009.Biogenetic barium distribution from the Upper Ordovician to Lower Silurian in the Yangtze area and its significance to paleoproductivity.Journal of Xi'an Shiyou University(Natural Science Edition),24(4):16-19]
郑和荣,高波,彭勇民,聂海宽,杨斐然.2013.中上扬子地区下志留统沉积演化与页岩气勘探方向.古地理学报,15(5):645-656.[Zheng H R,Gao B,Peng Y M,Nie H K,Yang F R.2013.Sedimentary evolution and shale gas exploration direction of the Lower Silurian in Middle-Upper Yangtze area.Journal of Palaeogeography(Chinese Edition),15(5):645-656]
邹才能,董大忠,王玉满,李新景,黄金亮,王淑芳,管全中,张晨晨,王红岩,刘洪林,拜文华,梁峰,吝文,赵群,刘德勋,杨智,梁萍萍,孙莎莎,邱振.2015.中国页岩气特征、挑战及前景(一).石油勘探与开发,42(6):689-701.[Zou C N,Dong D Z,Wang Y M,Li X J,Huang J L,Wang S F,Guan Q Z,Zhang C C,Wang H Y,Liu HL,Bai W H,Liang F,Lin W,Zhao Q,Liu D X,Yang Z,Liang P P,Sun S S,Qiu Z.2015.Shale gas in China:Characteristics,challenges and prospects(Ⅰ).Petroleum Exploration and Development,42(6):689-701]
Berner R A,Raiswell R.1983.Burial of organic carbon and pyrite sulfur in sediments over Phanerozoic time:A new theory.Geochimica et Cosmoshimica Acta,47(5):855-862.
Francois R,Hinjo S,Manganini S J,Ravizza G.1995.Bitgenetic barium fluxes to the deep sea:Implications for paleoproductivity reconstruction.Global Biogeochemical Cycles,9(2):289-303.
陈孝红,张保民,陈林,张国涛,李培军,张淼.2018.鄂西宜昌地区晚奥陶世-早志留世页岩气藏的主控地质因素与富集模式.地球学报,39(3):257-268.[Chen X H,Zhang B M,Chen L,Zhang G T,Li P J,Zhang M.2018.Main geological controlling factors and enrichment pattern of shale gas reservoirs in the Late OrdovicianEarly Silurian Strata of Yichang,Western Hubei Province.Acta Geoscientica Sinica,39(3):257-268]
陈旭,戎嘉余,周志毅,张元动,詹仁斌,刘建波,樊隽轩.2001.上扬子区奥陶-志留纪之交的黔中隆起和宜昌上升.科学通报,46(12):1052-1056.[Chen X,Rong J Y,Zhou Z Y,Zhang Y D,Zhan R B,Liu J B,Fan J X.2001.Qianzhong upheaval and Yichang rise formed at transition between the Ordovician and Silurian in Upper Yangtze Region.Chinese Science Bulletin,46(12):1052-1056]
陈旭,樊隽轩,王文卉,王红岩,聂海宽,石学文,文治东,陈冬阳,李文杰.2017.黔渝地区志留系龙马溪组黑色笔石页岩的阶段性渐进展布模式.中国科学:地球科学,47(6):720-732.[Chen X,Fan J X,Wang W H,Wang H Y,Nie H K,Shi X W,Wen Z D,Chen D Y,Li W J.2017.Stage-progressive distribution pattern of the Lungmachi black graptolitic shales from Guizhou to Chongqing,Central China.Science China Earth Science,47(6):720-732]
戴少武.2002.中扬子及邻区层序地层与原型盆地演化.石油与天然气地质,23(3):229-235.[Dai S W.2002.Stratigraphy sequences in the Middle Yangtze&adjacent region and evolution of prototype basins.Oil&Gas Geology,23(3):229-235]
樊隽轩,Melchin M J,陈旭,王怿,张元动,陈清,迟昭利,陈峰.2012.华南奥陶-志留系龙马溪组黑色笔石页岩的生物地层学.中国科学(地球科学),42(1):130-139.[Fan J X,Melchin M J,Chen X,Wang Y,Zhang Y D,Chen Q,Chi Z L,Chen F.2012.Biostratigraphy and geography of the Ordovician-Silurian Lungmachi black shales in South China.Scientia Sinica Terrae,42(1):130-139]
冯洪真,Erdtmann B D,王海峰.2000.上扬子区早古生代全岩Ce异常与海平面长缓变化.中国科学(D辑),30(1):66-72.[Feng H Z,Erdtmann B D,Wang H F.2000.Early Paleozoic whole-rock Ce anomalies and secular eustatic changes in the Upper Yangtze region.Science in China(Series D),30(1):66-72]
郭旭升,梅廉夫,汤济广,沈传波.2006.扬子地块中新生代构造演化对海相油气成藏的制约.石油与天然气地质,27(3):295-325.[Guo X S,Mei L F,Tang J G,Shen C B.2006.Constraint of MesoCenozonic tectonic evolution of Yangtze massif on formation of marine reseroirs.Oil&Gas Geology,27(3):295-325]
郭旭升.2014.南方海相页岩气“二元富集”规律:四川盆地及周缘龙马溪组页岩气勘探实践认识.地质学报,88(7):1209-1218.[Guo X S.2014.Rules of Two-Factor Enrichiment for marine shale gas in Southern China:Understanding from the Longmaxi Formation shale gas in Sichuan Basin and its surrounding area.Acta Geologica Sinica,88(7):1209-1218]
郭旭升,胡东风,魏志红,李宇平,魏祥峰.2016.涪陵页岩气田的发现与勘探认识.中国石油勘探,21(3):24-37.[Guo X S,Hu DF,Wei Z H,Li Y P,Wei X F.2016.Discovery and exploration of Fuling Shale Gas Field.China Petroleum Exploration,21(3):24-37]
何卫红,汪啸风,卜建军.2003.扬子海盆中部晚奥陶世五峰期海平面变化.地球学报,24(1):55-60.[He W H,Wang X F,Bu J J.2003.Sea-level change of the central Yangtze Sea Basin in the Late Ordovician Wufengian Period.Acta Geoscientica Sinica,24(1):55-60]
焦方正,冯建辉,易积正,蔡勋育,何发岐.2015.中扬子地区海相天然气勘探方向、关键问题与勘探对策.中国石油勘探,20(2):1-8.[Jiao F Z,Feng J H,Yi J Z,Cai X Y,He F Q.2015.Direction,key factors and solution of marine natural gas exploration in Yangtze Area.China Petroleum Exploration,20(2):1-8]
李双建,肖开华,沃玉进,龙胜祥,蔡立国.2008.南方海相上奥陶统-下志留统优质烃源岩发育的控制因素.沉积学报,26(5):872-880.[Li S J,Xiao K H,Wo Y J,Long S X,Cai L G.2008.Development controlling factors of Upper Ordovician-Lower Silurian high quality source rocks in marine sequence,South China.Acta Sedimentologica Sinica,26(5):872-880]
梁狄刚,郭彤楼,陈建平,边立曾,赵喆.2009a.中国南方海相生烃成藏研究的若干新进展(二):南方四套区域性海相烃源岩的地球化学特征.海相油气地质,14(1):1-15.[Liang D G,Guo T L,Chen J P,Bian L Z,Zhao Z.2009a.Some progresses on studies of hydrocarbon generation and accumulation in marine sedimentary regions,Southern China(Part 2):Geochemical characteristics of four suits of regional marine source rocks,South China.Marine Origin Petroleum Geology,14(1):1-15]
梁狄刚,郭彤楼,边立曾,陈建平,赵喆.2009b.中国南方海相生烃成藏研究的若干新进展(三):南方四套区域性海相烃源岩的沉积相及发育的控制因素.海相油气地质,14(2):1-19.[Liang DG,Guo T L,Bian L Z,Chen J P,Zhao Z.2009b.Some progresses on studies of hydrocarbon generation and accumulation in marine sedimentary regions,southern China(Part 3):Controlling factors on the sedimentary facies and development of Palaeozoic marine souce rocks.Marine Origin Petroleum Geology,14(2):1-19]
梁峰,王红岩,拜文华,郭伟,赵群,孙莎莎,张琴,武瑾,马超,雷治安.2017.川南地区五峰组-龙马溪组页岩笔石带对比及沉积特征.天然气工业,37(7):20-26.[Liang F,Wang H Y,Bai W H,Guo W,Zhao Q,Sun S S,Zhang Q,Wu J,Ma Chao,Lei Z A.2017.Graptolite correlation and sedimentary characteristics of Wufeng-Longmaxi shale in southern Sichuan Basin.Natural Gas Industry,37(7):20-26]
牟传龙,葛祥英,许效松,周恳恳,梁薇,王秀平.2014.中上扬子地区晚奥陶世岩相古地理及其油气地质意义.古地理学报,16(4):427-440.[Mou C L,Ge X Y,Xu X S,Zhou K K,Liang W,Wang X P.2014.Lithofacies palaeogeography of the Late Ordovician and its petroleum geological significance in Middle-Upper Yangtze Region.Journal of Palaeogeography(Chinese Edition),16(4):427-440]
牟传龙,王秀平,王启宇,周恳恳,梁薇,葛祥英,陈小炜.2016.川南及邻区下志留统龙马溪组下段沉积相与页岩气地质条件的关系.古地理学报,18(3):457-472.[Mou C L,Wang X P,Wang Q Y,Zhou K K,Liang W,Ge X Y,Chen X W.2016.Relationship between sedimentary facies and shale gas geological conditions of the Lower Silurian Longmaxi Formation in southern Sichuan Basin and its adjacent areas.Journal of Palaeogeography(Chinese Edition),18(3):457-472]
聂海宽,金之钧,马鑫,刘忠宝,林拓,杨振恒.2017.四川盆地及邻区上奥陶统五峰组-下志留统龙马溪组底部笔石带及沉积特征.石油学报,38(2):160-174.[Nie H K,Jin Z J,Ma X,Liu Z B,Lin T,Yang Z H.2017.Graptolites zone and sedimentary characteristics of Upper Ordovician Wufeng Formation-Lower Silurian Longmaxi Formation in Sichuan Basin and its adjacent areas.Acta Petrolei Sinica,38(2):160-174]
邱晓松,杨波,胡明毅.2013.中扬子地区五峰组-龙马溪组页岩气储层及含气性特征.天然气地球科学,24(6):1274-1283.[Qiu X S,Yang B,Hu M Y.2013.Characteristics of shale reservoirs and gas content of Wufeng-Longmaxi Formation in the middle Yangtze region.Natural Gas Geoscience,24(6):1274-1283]
苏文博,李志明,史晓颖,周洪瑞,黄思骥,刘晓茗,陈晓雨,张继恩,杨红梅,贾柳静,Huff W D,Elttensohn F R.2006.华南五峰组-龙马溪组与华北下马岭组的钾质斑脱岩及黑色岩系:两个地史转折期板块构造运动的沉积响应.地学前缘,13(6):82-95.[Su W B,Li Z M,Shi X Y,Zhou H R,Huang S J,Liu X M,Chen X Y,Zhang J E,Yang H M,Jia L J,Huff W D,Elttensohn F R.2006.K-bentonites and black shales from the Wufeng-Longmaxi Formations(Early Paleozoic,South China)and Xiamaling Formation(Early Neoproterozoic,North China):Implications for tectonic processes during two important transitions.Earth Science Frontiers,13(6):82-95]
孙小勇,牟传龙,葛祥英,王远翀,门欣.2016.四川广元-陕西镇巴地区上奥陶统五峰组地球化学特征及沉积环境意义.沉积与特提斯地质,36(1):46-54.[Sun X Y,Mou C L,Ge X Y,Wang YC,M X.2016.Geochemistry and sedimentary environments of the Upper Ordovician Wufeng Formation in Guangyuan,northern Sichuan and Zhenba,southern Shanxi.Sedimentary Geology and Tethyan Geology,36(1):46-54]
腾格尔,刘文汇,徐永昌.2005.海相地层无机参数与烃源岩发育环境的相关研究:以鄂尔多斯盆地为例.石油与天然气地质,26(4):411-421.[Tenger,Liu W H,Xu Y C.2005.Study on relation between inorganic parameters in marine deposits and developmental environment of hydrocarbon source rocks:Taking Ordos basin as an example.Oil&Gas Geology,26(4):411-421]
王清晨,严德天,李双建.2008.中国南方志留系底部优质烃源岩发育的构造-环境模式.地质学报,82(3):289-297.[Wang QC,Yan D T,Li S J.2008.Developmental controlling factors of Upper Ordovician-Lower Silurian high quality source rocks in marine sequence,South China.Acta Geologica Sinica,82(3):289-297]
王淑芳,邹才能,董大忠,王玉满,黄金亮,郭召杰.2014.四川盆地富有机质页岩硅质生物成因及对页岩气开发的意义.北京大学学报(自然科学版),50(3):476-486.[Wang S F,Zou C N,Dong D Z,Wang Y M,Huang J L,Guo Z J.2014.Biogenic silica of organic-rich shale in Sichuan Basin and its significance for shale gas.Acta Scientiarum Naturalium Universitatis Pekinensis,50(3):476-486]
王涛利,郝爱胜,陈清,李超,王庆涛,卢鸿,刘大永.2018.中扬子宜昌地区五峰组和龙马溪组页岩发育主控因素.天然气地球科学,29(5):616-631.[Wang T L,Hao A S,Chen Q,Li C,Wang Q T,Lu H,Liu D Y.2018.The study of main factors controlling the development of Wufeng Formation and Longmaxi Formation organicrich shales in the Yichang area,Middle Yangtze Region.Natural Gas Geoscience,29(5):616-631]
王怿,戎嘉余,詹仁斌,黄冰,吴荣昌,王光旭.2013.鄂西南奥陶系-志留系交界地层研究兼论宜昌上升.地层学杂志,37(3):264-274.[Wang Y,Rong J Y,Zhan R B,Huang B,Wu R C,Wang G X.2013.On the Ordovician-Silurian boundary strata in Southwest Hubei,and the Yichang Uplift.Journal of Stratigraphy,37(3):264-274]
王玉满,王淑芳,董大忠,李新景,黄金亮,张晨晨,管全中.2016.川南下志留统龙马溪组页岩岩相表征.地学前缘,23(1):119-133.[Wang Y M,Wang S F,Dong D Z,Li X J,Huang J L,Zhang CC,Guan Q Z.2016.Lithofacies characterization of Longmaxi Formation of the Lower Silurian,southern Sichuan.Earth Science Frontiers,23(1):119-133]
王玉满,李新景,董大忠,张晨晨,王淑芳.2017.上扬子地区五峰组-龙马溪组优质页岩沉积主控因素.天然气工业,37(4):9-20.[Wang Y M,Li X J,Dong D Z,Zhang C C,Wang S F.2017.Main factors controlling the sedimentation of high-quality shale in Wufeng-Longmaxi Fm,Upper Yangtze region.Natural Gas Industry,37(4):9-20]
王玉满,李新景,陈波,韩京,张家铭,袁飞,马杰,代兵,王浩,蒋珊.2018.中上扬子地区埃隆阶最厚斑脱岩层分布特征及地质意义.天然气地球科学,29(1):42-54.[Wang Y M,Li X J,Chen B,Han J,Zhang J M,Yuan F,Ma J,Dai B,Wang H,Jiang S.2018.Distribution characteristics and geological significance of the thickest Aeronian bentonite bed in Middle-Upper Yangtze Region.Natural Gas Geoscience,29(1):42-54]
王志刚.2015.涪陵页岩气勘探开发重大突破与启示.石油与天然气地质,36(1):1-6.[Wang Z G.2015.Breakthrough of Fuling shale gas exploration and development and its inspiration.Oil&Gas Geology,36(1):1-6]
吴蓝宇,陆永潮,蒋恕,刘晓峰,何贵松.2018.上扬子区奥陶系五峰组-志留系龙马溪组沉积期火山活动对页岩有机质富集程度的影响.石油勘探与开发,45(5):806-816.[Wu L Y,Lu Y C,Jiang S,Liu X F,He G S.2018.Effects of volcanic activities in Ordovician Wufeng-Silurian Longmaxi period on organic-rich shale in the Upper Yangtze area,South China.Petroleum Exploration and Development,45(5):806-816]
熊国庆,王剑,李园园,余谦,门玉澎,周小琳,熊小辉,周业鑫,杨潇.2017.大巴山地区早古生代黑色岩系岩相古地理及页岩气地质意义.古地理学报,19(6):965-986.[Xiong G Q,Wang J,Li Y Y,Yu Q,Men Y P,Zhou X L,Xiong X H,Zhou Y X,Yang X.2017.Lithofacies palaeogeography of the Early Paleozoic black rock series in Dabashan region and their shale-gas geological significance.Journal of Palaeogeography(Chinese Edition),19(6):965-986]
严德天,王清晨,陈代钊,汪建国,王卓卓.2008.扬子及周缘地区上奥陶统-下志留统烃源岩发育环境及其控制因素.地质学报,82(3):321-327.[Yan D T,Wang Q C,Chen D Z,Wang J G,Wang Z Z.2008.Sedimentary environment and development controls of the hydrocarbon sources beds:The Upper Ordovician Wufeng Formation and the Lower Silurian Longmaxi Formation in the Yangtze Area.Acta Geologica Sinica,82(3):321-327]
严德天,汪建国,王卓卓.2009.扬子地区上奥陶-下志留统生物钡特征及其古生产力意义.西安石油大学学报(自然科学版),24(4):16-19.[Yan D T,Wang J G,Wang Z Z.2009.Biogenetic barium distribution from the Upper Ordovician to Lower Silurian in the Yangtze area and its significance to paleoproductivity.Journal of Xi'an Shiyou University(Natural Science Edition),24(4):16-19]
郑和荣,高波,彭勇民,聂海宽,杨斐然.2013.中上扬子地区下志留统沉积演化与页岩气勘探方向.古地理学报,15(5):645-656.[Zheng H R,Gao B,Peng Y M,Nie H K,Yang F R.2013.Sedimentary evolution and shale gas exploration direction of the Lower Silurian in Middle-Upper Yangtze area.Journal of Palaeogeography(Chinese Edition),15(5):645-656]
邹才能,董大忠,王玉满,李新景,黄金亮,王淑芳,管全中,张晨晨,王红岩,刘洪林,拜文华,梁峰,吝文,赵群,刘德勋,杨智,梁萍萍,孙莎莎,邱振.2015.中国页岩气特征、挑战及前景(一).石油勘探与开发,42(6):689-701.[Zou C N,Dong D Z,Wang Y M,Li X J,Huang J L,Wang S F,Guan Q Z,Zhang C C,Wang H Y,Liu HL,Bai W H,Liang F,Lin W,Zhao Q,Liu D X,Yang Z,Liang P P,Sun S S,Qiu Z.2015.Shale gas in China:Characteristics,challenges and prospects(Ⅰ).Petroleum Exploration and Development,42(6):689-701]
Berner R A,Raiswell R.1983.Burial of organic carbon and pyrite sulfur in sediments over Phanerozoic time:A new theory.Geochimica et Cosmoshimica Acta,47(5):855-862.
Francois R,Hinjo S,Manganini S J,Ravizza G.1995.Bitgenetic barium fluxes to the deep sea:Implications for paleoproductivity reconstruction.Global Biogeochemical Cycles,9(2):289-303.
© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号 地址：北京市海淀区学院路29号 邮编：100083 电话：办公室：(+86 10)66554848；文献借阅、咨询服务、科技查新：66554700 |