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扬子陆块下古生界页岩发育特征与沉积模式

徐政语 蒋恕 熊绍云 梁兴 王高成 郭燕玲 何勇 饶大骞

徐政语, 蒋恕, 熊绍云, 梁兴, 王高成, 郭燕玲, 何勇, 饶大骞. 扬子陆块下古生界页岩发育特征与沉积模式[J]. 沉积学报, 2015, 33(1): 21-35. doi: 10.14027/j.cnki.cjxb.2015.01.003
引用本文: 徐政语, 蒋恕, 熊绍云, 梁兴, 王高成, 郭燕玲, 何勇, 饶大骞. 扬子陆块下古生界页岩发育特征与沉积模式[J]. 沉积学报, 2015, 33(1): 21-35. doi: 10.14027/j.cnki.cjxb.2015.01.003
XU ZhengYu, JIANG Shu, XIONG ShaoYun, LIANG Xing, WANG GaoCheng, GUO YanLing, HE Yong, RAO DaQian. Characteristics and Depositional Model of the Lower Paleozoic Organic Rich Shale in the Yangtze Continental Block[J]. Acta Sedimentologica Sinica, 2015, 33(1): 21-35. doi: 10.14027/j.cnki.cjxb.2015.01.003
Citation: XU ZhengYu, JIANG Shu, XIONG ShaoYun, LIANG Xing, WANG GaoCheng, GUO YanLing, HE Yong, RAO DaQian. Characteristics and Depositional Model of the Lower Paleozoic Organic Rich Shale in the Yangtze Continental Block[J]. Acta Sedimentologica Sinica, 2015, 33(1): 21-35. doi: 10.14027/j.cnki.cjxb.2015.01.003

扬子陆块下古生界页岩发育特征与沉积模式

doi: 10.14027/j.cnki.cjxb.2015.01.003
基金项目: 国家重大科技专项(编号:2015ZX05068)、中国石油天然气集团公司重大科技项目(编号:2012F-47-02)与中国石油天然气股份公司科技项目(编号:2012B-0504)基金联合资助
详细信息
    作者简介:

    徐政语 男 1964年出生 博士 高级工程师 构造地质学与石油地质学 E-mail:Xuzy_hz@petrochina.com.cn

  • 中图分类号: P512.2;P595

Characteristics and Depositional Model of the Lower Paleozoic Organic Rich Shale in the Yangtze Continental Block

  • 摘要: 为了深入探讨扬子陆块下古生界页岩发育与分布特征、建立沉积模式,系统收集与整理了扬子陆块下寒武统牛蹄塘组与上奥陶统—下志留统五峰—龙马溪组两套富有机质页岩大量数据,选取贵州省三都县渣拉沟及四川省筠连县昭104井两个典型剖面与井岩芯进行了系统观察与采样,对扬子陆块范围内两套富有机质页岩岩性与沉积相发育特征进行了系统分析.研究表明,早古生代以来,扬子陆块受被动大陆边缘扩张与陆缘造山挠曲坳陷两类成盆环境影响[1-2],牛蹄塘组页岩沉积于被动大陆边缘扩张环境,缘于上升洋流与缺氧事件复合沉积模式,富有机质页岩以扬子陆块东南缘深水陆棚—斜坡相区最为发育、厚度最大、有机碳含量最高;五峰—龙马溪组页岩沉积于加里东期周缘前陆造山环境,缘于浅水陆棚—闭塞滞留海湾沉积模式,富有机质页岩以中上扬子陆块东南缘深水陆棚区最为发育、厚度最大、有机碳含量最高.
  • [1] 余达淦,管太阳,黄国夫. 华南(东)晋宁—加里东海盆地形成、演化及封闭[J]. 华东地质学院学报,1993,16(4):301-319.[Yu Dagan, Guan Taiyang, Huang Guofu. The formation, evolution and closure of Jinning-Caledonian Sea Basin in the East of Huanan[J]. Journal of East China Geological Institute, 1993, 16(4): 301-319.]
    [2] 苏文博,李志明,Ettensohn F R,等. 华南五峰组—龙马溪组黑色岩系时空展布的主控因素及其启示[J]. 地球科学,2007,32(6):819-827.[Su Wenbo, Li Zhiming,Ettensohn F R, et al. Distribution of black shale in the Wufeng-Longmaxi Formations(Ordovician-Silurian), South China: Major controlling factors and implications[J]. Earth Science, 2007, 32(6): 819-827.]
    [3] Dapples E C, Rominger J F. Orientation analysis of fine-grained clastic sediments:a report of progress[J]. The Journal of Geology, 1945, 53(4): 246-261.
    [4] Dill R F, Dietz R S, Stewart H. Deep-sea channels and delta of the Monterey submarine canyon[J]. Geological Society of America Bulletin,1954, 65(2): 191-194.
    [5] Sullwold H H Jr. Tarzana fan, deep submarine fan of late Miocene age Los Angeles County, California[J]. AAPG Bulletin, 1960, 44(4): 433-457.
    [6] Kuenen P H. Properties of turbidity currents of high density[J]. Society of Economic Paleontologists and Mineralogists, 1951, (2): 14-33.
    [7] van Straaten L M J U, Kuenen P H. Tidal action as a cause of clay accumulation[J]. Journal of SedimentaryResearch, 1958, 28(4): 406-413.
    [8] Webb J B. Geological history of plains of western Canada[J]. AAPG Bulletin, 1951, 35(11): 2291-2315.
    [9] Dellwig L F. Origin of the salina salt of Michigan[J]. Journal of Sedimentary Research, 1955, 25(2): 83-110.
    [10] Radczewski O E. Eolian deposits in marine sediments: Part 6. Special features of sediments[J]. AAPG Special Volumes, 1939, 142: 496-502.
    [11] Picard M D. Classification of fine-grained sedimentary rocks [J]. Journal of Sedimentary Research, 1971, 41(1): 179-195.
    [12] Lundegard P D, Samuels N D. Field classification of fine-grained sedimentary rocks[J]. Journal of Sedimentary Research, 1980, 50(3): 781-786.
    [13] Schubel J R, Kana T W. Agglomeration of fine-grained suspended sediment in Northern Chesapeake Bay[J]. Powder Technology, 1972, 6(1): 9-16.
    [14] Stow D A V, Piper D J W. Deep-water fine-grained sediments: facies models[J]. Geological Society, London, Special Publications, 1984, 15: 611-646.
    [15] McCave I N. Deposition of fine-grained suspended sediment from tidal currents[J]. Journal of Geophysical Research, 1970, 75(21): 4151-4159.
    [16] Lick W. Entrainment, deposition,and transport of fine-grained sediments in lakes[J]. Sediment/Freshwater Interaction: Developments in Hydrobiology, 1982, 9: 31-40.
    [17] Kranck K. Experiments on the significance of flocculation in the settling of fine-grained sediment in still water[J]. Canadian Journal of Earth Sciences, 1980, 17(11): 1517-1526.
    [18] McCave I N, Swift S A. A physical model for the rate of deposition of fine-grained sediments in the deep sea[J]. Geological Society of America Bulletin, 1976, 87(4): 541-546.
    [19] Stow D A V, Bowen A J. A physical model for the transport and sorting of fine-grained sediment by turbidity currents[J]. Sedimentology, 1980, 27(1): 31-46.
    [20] Jones K P N, McCave I N, Patel D. A computer-interfaced sedigraph for modal size analysis of fine-grained sediment[J]. Sedimentology, 1988, 35(1): 163-172.
    [21] McCave I N. Mechanics of deposition of fine-grained sediments from nepheloid layers [J]. Geo-Marine Letters, 1984-1985, 4(3/4): 243-245.
    [22] Wignall P B. Model for transgressive black shales? [J]. Geology, 1991, 19(2): 167-170.
    [23] Bennett R H, Bryant W R, Hulbert M H, et al. Microstructure of Fine-Grained Sediments: From Mud to Shale[M]. Berlin, Heidelberg: Springer-Verleg, 1991.
    [24] Arthur M A, Dean W E, Stow D A V. Models for the deposition of Mesozoic-Cenozoic fine-grained organic-carbon-rich sediment in the deep sea[J]. Geological Society, London, Special Publications, 1984, 15: 527-560.
    [25] Loucks R G, Ruppel S C. Mississippian Barnett Shale: lithofacies and depositional setting of a deep water shale gas succession in the Fort Worth Basin, Texas [J]. AAPG Bulletin, 2007, 91(4): 579-601.
    [26] Van Cappellen P, Ingall E D. Benthic phosphorus regeneration, net primary production, and ocean anoxia: A model of the coupled marine biogeochemical cycles of carbon and phosphorus[J]. Paleoceanography, 1994, 9(5): 677-692.
    [27] Erbacher J, Huber B T, Norris R D, et al. Increased thermohaline stratification as a possible cause for an ocean anoxic event in the Cretaceous period [J]. Nature, 2001, 409(6818): 325-327.
    [28] Stow D A V, Tabrez A R. Hemipelagites: processes, facies and model[J]. Geological Society, London, Special Publications, 1998, 129: 317-337.
    [29] Stow D A V, Huc A Y, Bertrand P. Depositional processes of black shales in deep water[J]. Marine and Petroleum Geology, 2001, 18(4): 491-498.
    [30] Wijsman J W M, Herman P M J, Middelburg J J, et al. A model for early diagenetic processes in sediments of the continental shelf of the Black Sea[J]. Estuarine, Coastal and Shelf Science, 2002, 54(3): 403-421.
    [31] Leckie D A, Singh C, Goodarzi F, et al. Organic-rich, radioactive marine shale: a case study of a shallow-water condensed section, Cretaceous shaftesbury formation, Alberta, Canada [J]. Journal of Sedimentary Research, 1990, 60(1): 101-117.
    [32] Egenhoff S O, Fishman N S. Traces in the dark-sedimentary processes and facies and gradients in the upper shale member of the upper Devonian-Lower Mississippian Bakken formation, Willistion basin, North Dakota,U.S.A[J]. Journal of Sedimentary Research, 2013, 83(9): 803-824.
    [33] Lehmann D, Brett C E, Cole R,et al. Distal sedimentation in a peripheral foreland basin: Ordovician black shales and associated flysch of the western Taconic foreland, New York State and Ontario[J]. Geological Society of America Bulletin, 1995, 107(6): 708-724.
    [34] Piasecki S, Christiansen F G, Stemmerik L. Depositional history of an Upper Carboniferous organic-rich lacustrine shale from East Greenland[J]. Bulletin of Canadian Petroleum Geology, 1990, 38(3): 273-287.
    [35] Giles J M, Soreghan M J, Benison K C, et al. Lakes, loess, and paleosols in the permian wellington formation of Oklahoma, U.S.A.: implications for paleoclimate and paleogeography of the Midcontinent [J]. Journal of Sedimentary Research, 2013, 83(10): 825-846.
    [36] 卢衍豪. 中国寒武纪沉积矿产与“生物—环境控制论”[M]. 北京:地质出版社,1979.[Lu Yanhao. China Cambrian Sedimentary Minerals and “Biological Environment Control Theory”[M]. Beijing: Geological Publishing House, 1979.]
    [37] 黄志诚,黄钟瑾,陈智娜. 下扬子区五峰组火山碎屑岩与放射虫硅质岩[J]. 沉积学报,1991,9(2):1-14.[Huang Zhicheng, Huang Zhongjin, Chen Zhina. Volcanic rock and radiolarian silicilith of Wufeng Formarion in Lower Yangtze region[J]. Acta Sedimentologica Sinica, 1991, 9(2): 1-14.]
    [38] 姜月华,岳文浙,业治铮. 华南下古生界缺氧事件与黑色页岩及有关矿产[J]. 有色金属矿产与勘查,1994,3(5):272-278.[Jiang Yuehua, Yue Wenzhe, Ye Zhizheng. Anoxic event, black shales and related mineral resources: Taking the Lower Palaeozoic in southern China as an example[J]. Geological Exploration for Non-ferrous Metals, 1994, 3(5): 272-278.]
    [39] 苏文博,何龙清,王永标,等. 华南奥陶—志留系五峰组及龙马溪组底部斑脱岩与高分辨综合地层[J]. 中国科学(D辑):地球科学,2002,32(3):207-219.[Su Wenbo, He Longqing, Wang Yongbiao, et al. Southern China Ordovician-Silurian Wufeng and Longmaxi Formation at the bottom of bentonite with high resolution[J]. Science China(Seri. D): Earth Sciences, 2002, 32(3): 207-219.]
    [40] 冯增昭. 中国寒武纪和奥陶纪岩相古地理[M]. 北京:石油工业出版社,2004.[Feng Zengzhao. China Cambrian and Ordovician Lithofacies Paleogeography[M]. Beijing: Petroleum Industry Press, 2004.]
    [41] 马永生,陈洪德,王国力,等.中国南方层序地层与古地理[M]. 北京:科学出版社,2009:1-584.[Ma Yongsheng, Chen Hongde, Wang Guoli, et al. China Southern Sequence Stratigraphy and Paleogeography [M]. Beijing: Science Press, 2009: 1-584.]
    [42] 董大忠,程克明,王玉满,等.中国上扬子区下古生界页岩气形成条件及特征.石油与天然气地质[J],2010,31(3):288-299.[Dong Dazhong, Cheng Keming, Wang Yuman, et al. Forming conditions and characteristics of shale gas in the Lower Paleozoic of the Upper Yangtze region, China[J]. Oil & Gas Geology, 2010, 31(3): 288-299.]
    [43] 潘继平,乔德武,李世臻,等. 下扬子地区古生界页岩气地质条件与勘探前景[J]. 地质通报,2011,30(2/3):337-343.[Pan Jiping, Qiao Dewu, Li Shizhen, et al. Shale-gas geological conditions and exploration prospect of the Paleozoic marine strata in Lower Yangtze area, China[J]. Geological Bulletin of China, 30(2/3): 337-343.]
    [44] 李任伟,卢家烂,张淑坤,等. 震旦纪和早寒武世黑色页岩有机碳同位素组成[J]. 中国科学(D辑):地球科学,1999,29(4):351-357.[Li Renwei, Lu Jialan, Zhang Shukun, et al. Sinian and Early Cambrian black shale organic carbon isotope composition[J]. Science China (Seri. D): Earth Sciences, 1999, 29(4): 351-357.]
    [45] 吕炳全,王红罡,胡望水,等. 扬子地块东南古生代上升流沉积相及其与烃源岩的关系[J]. 海洋地质与第四纪地质,2004,24(4):29-35.[Lü Bingquan,Wang Honggang, Hu Wangshui, et al. Relationship between Paleozoic upwelling facies and hydrocarbon in Southeastern marginal Yangtze block[J]. Marine Geology & Quaternary Geology, 2004, 24(4): 29-35.]
    [46] 赵明胜,王约,田景春,等. 从生物化石组合特征剖析黑色页岩的沉积环境——以鄂西长阳地区寒武系牛蹄塘组为例[J]. 中国地质,2013,40(5):1484-1492.[Zhao Mingsheng, Wang Yue, Tian Jingchun, et al. Asedimentary environment analysis of black shales based on fossil assemblage characteristics: A case study of Cambrian Niutitang Formation in Changyang area, western Hubei[J]. Geology in China, 2013, 40(5): 1484-1492.]
    [47] 张海全,许效松,刘伟,等. 中上扬子地区晚奥陶世—早志留世岩相古地理演化与黑色页岩的关系[J]. 沉积与特提斯地质,2013,33(2):17-24.[Zhang Haiquan, Xu Xiaosong, Liu Wei, et al. Late Ordovician-Early Silurian sedimentary facies and palaeogeographic evolution and its bearings on the black shales in the Middle-Upper Yangtze area[J]. Sedimentary Geology and Tethyan Geology, 2013, 33(2): 17-24.]
    [48] 粱狄刚,郭彤楼,边立曾,等. 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[J]. 海相油气地质,2009,14(2):1-19.[Liang Digang ,Guo Tonglou, Bian Lizeng, et al. 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 source rocks[J]. Marine Petroleum Geology, 2009, 14(2): 1-19.]
    [49] 汪正江,王剑,卓皆文,等. 扬子陆块震旦纪—寒武纪之交的地壳伸展作用:来自沉积序列与沉积地球化学证据[J]. 地质论评,2011,57(5):731-742.[Wang Zhengjiang,Wang Jian, Zhuo Jiewen, et al. Crust extensional activity during the transition from Sinian(Ediacaran)to Cambrian in Yangtze Block: Evidence from the depositional Sequence and geochemistry[J]. Geological Review, 2011, 57(5): 731-742.]
    [50] 李志明,全秋琦. 中国南部奥陶—志留纪笔石页岩相类型及其构造古地理[J]. 地球科学,1992,17(3):261-269.[Li Zhiming, Quan Qiuqi. Geography of Ordovician and Silurian graptolite-bearing strata in South China[J]. Earth Science, 1992, 17(3): 261-269.]
    [51] 程立雪,王元君,陈洪德,等. 上扬子地区震旦系—早古生界黑色页岩的沉积和埋藏环境[J]. 岩石学报,2013,29(8):2906-2912.[Cheng Lixue, Wang Yuanjun, Chen Hongde, et al. Sedimentary and burial environment of black shales of Sinian to Early Palaeozoic in Upper Yangtze region[J]. Acta Petrologica Sinica,2013,29(8):2906-2912.]
    [52] 周明忠,罗泰义,李正祥,等. 遵义牛蹄塘组底部凝灰岩锆石SHRIMP U-Pb年龄及其地质意义[J]. 科学通报,2008,53(1):104-110.[Zhou Mingzhong, Luo Taiyi, Li Zhengxiang, et al. Bottom of Zunyi Niutitang Formation tuff zircon SHRIMP U-Pb age and its geological significance[J]. Chinese Science Bulletin, 2008, 53(1): 104-110.]
    [53] 闫剑飞,余谦,刘伟,等. 中上扬子地区下古生界页岩气资源前景分析[J]. 沉积与特提斯地质,2010,30(3):96-103.[Yan Jianfei, Yu Qian, Liu Wei, et al. Perspectives of the Lower Palaeozoic shale gas resources in the Middle-Upper Yangtze area[J]. Sedimentary Geology and Tethyan Geology, 2010, 30(3): 96-103.]
    [54] 王兰生,邹春艳,郑平,等. 四川盆地下古生界存在页岩气的地球化学依据[J]. 天然气工业,2009,29(5):59-62.[Wang Lansheng, Zou Chunyan, Zheng Ping, et al. Geochemical evidence of shale gas existed in the Lower Paleozoic Sichuan Basin[J]. Natural Gas Industry, 2009, 29(5): 59-62.]
    [55] 孙玮,刘树根,冉波,等. 四川盆地及周缘地区牛蹄塘组页岩气概况及前景评价[J]. 成都理工大学学报:自然科学版,2012,39(2):170-175.[Sun Wei, Liu Shugen, Ran Bo, et al. General situation and prospect evaluation of the shale gas in Niutitang Formation of Sichuan Basin and its surrounding areas[J]. Journal of Chengdu University of Technology: Science & Technology Edition, 2012, 39(2): 170-175.]
    [56] 王丽波,久凯,曾维特,等. 上扬子黔北地区下寒武统海相黑色泥页岩特征及页岩气远景区评价[J]. 岩石学报,2013,29(9):3263-3278.[Wang Libo, Jiu Kai, Zeng Weite, et al. Characteristics of Lower Cambrian marine black shales and evaluation of shale gas prospective area in Qianbei area, Upper Yangtze region[J]. Acta Petrologica Sinica, 2013, 29(9): 3263-3278.]
    [57] 胡琳,朱炎铭,陈尚斌,等. 中上扬子地区下寒武统筇竹寺组页岩气资源潜力分析[J]. 煤炭学报,2012,37(11):1871-1877.[Hu Lin, Zhu Yanming, Chen Shangbin, et al. Resource potential analysis of shale gas in Lower Cambrian Qiongzhusi Formation in Middle & Upper Yangtze region[J]. Journal of China Coal Society, 2012, 37(11): 1871-1877.]
    [58] 郭彤楼,张汉荣. 四川盆地焦石坝页岩气田形成与富集高产模式[J]. 石油勘探与开发,2014,41(1):28-36.[Guo Tonglou, Zhang Hanrong. Formation and enrichment mode of Jiaoshiba shale gas field, Sichuan Basin[J]. Petroleum Exploration and Development, 2014, 41(1): 28-36.]
    [59] 袁宏,肖加飞,何熙琦,等. 黔北牛蹄塘组的地球化学特征及形成环境[J]. 贵州地质,2007,24(1):55-63.[Yuan Hong, Xiao Jiafei, He Xiqi, et al. Geochemical characteristics and formation environment of the Niutitang Formation in the North Guizhou[J]. Guizhou Geology, 2007, 24(1): 55-63.]
    [60] 姜月华,岳文浙,业治铮. 中国南方下寒武统石煤的特征、沉积环境和成因[J]. 中国煤田地质,1994,6(4):26-31.[Jiang Yuehua, Yue Wenzhe, Ye Zhizheng. Characteristics, sedimentary environment and origin of the Lower Cambrian stone-like coal in Southern China[J]. China Coal Geology, 1994, 6(4):26-31.]
    [61] 吴朝东. 湘西震旦—寒武纪交替时期古海洋环境的恢复[J]. 地学前缘,2000,7(增刊):45-57.[Wu Chaodong. Recovery of the Paleo-ocean environment in the alternating epoch of Late Sinian and Early Cambrian in the West Hunan[J]. Earth Science Frontiers, 2000, 7(Suppl.): 45-57.]
    [62] 李有禹. 湖南大庸慈利一带下寒武统黑色页岩中海底喷流沉积硅岩的地质特征[J]. 岩石学报,1997,13(1):121-126.[Li Youyu. The geological characteristics of sea-floor exhalation sedimentary chert in Lower Cambrian Black Shales in Dayong-Cili area,Hunan province[J]. Acta Petrologica Sinica, 1997, 13(1): 121-126.]
    [63] 李娟,于炳松,郭峰. 黔北地区下寒武统底部黑色页岩沉积环境条件与源区构造背景分析[J]. 沉积学报,2013,31(1):20-31.[Li Juan, Yu Bingsong, Guo Feng. Depositional setting and tectonic background analysis on Lower Cambrian black shales in the north of Guizhou province[J]. Acta Sedimentologica Sinica, 2013, 31(1): 20-31.]
    [64] 魏怀瑞,杨瑞东,鲍淼,等. 贵州早寒武世黑色页岩地球化学特征及其意义[J]. 贵州大学学报:自然科学版,2007,23(4):356-360.[Wei Huairui, Yang Ruidong, Bao Miao, et al. Geochemical characteristics of Early Cambrian black shale in Guizhou province, China [J]. Journal of Guizhou University: Natural Science Edition, 2007, 23(4): 356-360.]
    [65] 吴朝东,杨承运,陈其英. 湘西黑色岩系地球化学特征和成因意义[J]. 岩石矿物学杂志,1999,18(1):26-39.[Wu Chaodong, Yang Chengyun, Chen Qiying. The origin and geochemical characteristics of Upper Sinain-Lower Cambrian black shales in western Hunan[J]. Acta Petrologica et Mineralogical, 1999, 18(1): 26-39.]
    [66] 杨恩林,吕新彪,鲍淼,等. 黔东下寒武统黑色页岩微量元素的富集及成因分析[J]. 地球科学进展,2013,28(10):1160-1169.[Yang Enlin, Lü Xinbiao, Bao Miao, et al. Enrichment and origin of some trace elements in black shales from the Early Cambrian in Eastern Guizhou province[J]. Advances in Earth Science, 2013, 28(10): 1160-1169.]
    [67] 陈旭,张元动,樊隽轩,等. 广西运动的进程:来自生物相和岩相带的证据[J]. 中国科学(D辑):地球科学,2012,42(11):1617-1626.[Chen Xu, Zhang Yuandong, Fan Junxuan, et al. Process of Guangxi movement: Evidence from biological phase and facies belts [J]. Science China(Seri. D): Earth Sciences, 2012, 42(11): 1617-1626.]
    [68] 刘树根,王世玉,孙玮,等. 四川盆地及其周缘五峰组龙马溪组黑色页岩特征[J]. 成都理工大学学报:自然科学版,2013,40(6):621-639.[Liu Shugen, Wang Shiyu, Sun Wei, et al. Characteristics of block shale in Wufeng Formation and Longmaxi Formation in Sichuan Basin and its peripheral areas[J]. Journal of Chengdu University of Technology: Science and Technology Edition, 2013, 40(6): 621-639.]
    [69] 陈旭,戎嘉余. 从生物地层学到大地构造学——以华南奥陶系和志留系为例[J]. 现代地质,1999,13(4):385-389.[Chen Xu, Rong Jiayu. From biostratigraphy to tectonics—with Ordovician and Silurian of South China as an example[J]. Geoscience, 1999, 13(4): 385-389.]
    [70] 严德天,陈代钊,王清晨,等. 扬子地区奥陶系—志留系界线附近地球化学研究[J]. 中国科学(D辑):地球科学,2009,39(3):285-299.[Yan Detian, Chen Daizhao, Wang Qingchen, et al. Geochemical study of Yangtze Ordovician- Silurian boundary[J]. Science China(Seri. D): Earth Sciences, 2009, 39(3): 285-299.]et al. Geochemical evidence of shale gas existed in the Lower Paleozoic Sichuan Basin[J]. Natural Gas Industry, 2009, 29(5): 59-62.]
    [71] 孙玮,刘树根,冉波,等. 四川盆地及周缘地区牛蹄塘组页岩气概况及前景评价[J]. 成都理工大学学报: 自然科学版,2012,39(2): 170-175.[Sun Wei, Liu Shugen, Ran Bo, et al. General situation and prospect evaluation of the shale gas in Niutitang Formation of Sichuan Basin and its surrounding areas[J]. Journal of Chengdu University of Technology: Science & Technology Edition, 2012, 39(2): 170-175.]
    [72] 王丽波,久凯,曾维特,等. 上扬子黔北地区下寒武统海相黑色泥页岩特征及页岩气远景区评价[J]. 岩石学报,2013,29(9): 3263-3278.[Wang Libo, Jiu Kai, Zeng Weite, et al. Characteristics of Lower Cambrian marine black shales and evaluation of shale gas prospective area in Qianbei area, Upper Yangtze region[J]. Acta Petrologica Sinica, 2013, 29(9): 3263-3278.]
    [73] 胡琳,朱炎铭,陈尚斌,等. 中上扬子地区下寒武统筇竹寺组页岩气资源潜力分析[J]. 煤炭学报,2012,37(11): 1871-1877.[Hu Lin, Zhu Yanming, Chen Shangbin, et al. Resource potential analysis of shale gas in Lower Cambrian Qiongzhusi Formation in Middle & Upper Yangtze region[J]. Journal of China Coal Society, 2012, 37(11): 1871-1877.]
    [74] 郭彤楼,张汉荣. 四川盆地焦石坝页岩气田形成与富集高产模式[J]. 石油勘探与开发,2104,41(1): 28-36.[Guo Tonglou, Zhang Hanrong. Formation and enrichment mode of Jiaoshiba shale gas field, Sichuan Basin[J]. Petroleum Exploration and Development, 2014, 41(1): 28-36.]
    [75] 袁宏,肖加飞,何熙琦,等. 黔北牛蹄塘组的地球化学特征及形成环境[J]. 贵州地质,2007,24(1): 55-63.[Yuan Hong, Xiao Jiafei, He Xiqi, et al. Geochemical characteristics and formation environment of the Niutitang formation in the North Guizhou[J]. Guizhou Geology, 2007, 24(1): 55-63.]
    [76] 姜月华,岳文浙,业治铮. 中国南方下寒武统石煤的特征、沉积环境和成因[J]. 中国煤田地质,1994,6(4): 26-31.[Jiang Yuehua, Yue Wenzhe, Ye Zhizheng. Characteristics, sedimentary environment and 0rigin of the Lower Cambrian stone-like coal in Southern China[J]. China Coal Geology, 1994, 6(4):26-31.]
    [77] 吴朝东. 湘西震旦—寒武纪交替时期古海洋环境的恢复[J]. 地学前缘,2000,7(增刊): 45-57.[Wu Chaodong. Recovery of the Paleo-ocean environment in the alternating epoch of late Sinia and early Cambrian in the west Hunan[J]. Earth science Frontiers, 2000, 7(Suppl.): 45-57.]
    [78] 李有禹. 湖南大庸慈利一带下寒武统黑色页岩中海底喷流沉积硅岩的地质特征[J]. 岩石学报,1997,13(1): 121-126.[Li Youyu. The geological characteristics of sea-floor exhalation sedimentary chert in Lower Cambrian Black Shales in Dayong-Cili area,Hunan province[J]. Acta Petrologica Sinica, 1997, 13(1): 121-126.]
    [79] 李娟,于炳松,郭峰. 黔北地区下寒武统底部黑色页岩沉积环境条件与源区构造背景分析[J]. 沉积学报,2013,31(1): 20-31.[Li Juan, Yu Bingsong, Guo Feng. Depositional setting and tectonic background analysis on Lower Cambrian black shales in the North of Guizhou province[J]. Acta Sedimentologica Sinica, 2013, 31(1): 20-31.]
    [80] 魏怀瑞,杨瑞东,鲍淼,等. 贵州早寒武世黑色页岩地球化学特征及其意义[J]. 贵州大学学报: 自然科学版,2007,23(4): 356-360.[Wei Huairui, Yang Ruidong, Bao Miao, et al. Geochemical characteristics of Early Cambrian black shale in Guizhou province, China [J]. Journal of Guizhou University: Natural Science Edition, 2007, 23(4): 356-360.]
    [81] 吴朝东,杨承运,陈其英. 湘西黑色岩系地球化学特征和成因意义[J]. 岩石矿物学杂志,1999,18(1): 26-39.[Wu Chaodong, Yang Chengyun, Chen Qiying. The origin and geochemical characteristics of Upper Sinain-Lower Cambrian black shales in western Hunan[J]. Acta Petrologica et Mineralogical, 1999, 18(1): 26-39.]
    [82] 杨恩林,吕新彪,鲍淼,等. 黔东下寒武统黑色页岩微量元素的富集及成因分析[J]. 地球科学进展,2013,28(10): 1160-1169.[Yang Enlin, Lü Xinbiao, Bao Miao, et al. Enrichment and origin of some trace elements in black shales from the Early Cambrian in Eastern Guizhou province[J]. Advances in Earth Science, 2013, 28(10): 1160-1169.]
    [83] 陈旭,张元动,樊隽轩,等. 广西运动的进程: 来自生物相和岩相带的证据[J]. 中国科学(D辑): 地球科学,2012,42(11): 1617-1626.[Chen Xu, Zhang Yuandong, Fan Junxuan, et al. Process of Guangxi movement: Evidence from biological phase and facies belts [J]. Science China(Series D): Earth Sciences, 2012, 42(11): 1617-1626.]
    [84] 刘树根,王世玉,孙玮,等. 四川盆地及其周缘五峰组龙马溪组黑色页岩特征[J]. 成都理工大学学报: 自然科学版,2013,40(6): 621-639.[Liu Shugen, Wang Shiyu, Sun Wei, et al. Characteristics of block shale in Wufeng Formation and Longmaxi Formation in Sichuan Basin and its peripheral areas[J]. Journal of Chengdu University of Technology: Science and Technology Edition, 2013, 40(6): 621-639.]
    [85] 陈旭,戎嘉余. 从生物地层学到大地构造学——以华南奥陶系和志留系为例[J]. 现代地质,1999,13(4): 385-389.[Chen Xu, Rong Jiayu. From biostratigraphy to tectonics—with Ordovician and Silurian of South China as an example[J]. Geoscience, 1999, 13(4): 385-389.]
    [86] 严德天,陈代钊,王清晨,等. 扬子地区奥陶系—志留系界线附近地球化学研究[J]. 中国科学(D辑): 地球科学,2009,39(3): 285-299.[Yan Detian, Chen Daizhao, Wang Qingchen, et al. Geochemical study of Yangtze Ordovician - Silurian boundary near[J]. Science China(Series D): Earth Sciences, 2009, 39(3): 285-299.]
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  • 收稿日期:  2014-02-24
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目录

    扬子陆块下古生界页岩发育特征与沉积模式

    doi: 10.14027/j.cnki.cjxb.2015.01.003
      基金项目:  国家重大科技专项(编号:2015ZX05068)、中国石油天然气集团公司重大科技项目(编号:2012F-47-02)与中国石油天然气股份公司科技项目(编号:2012B-0504)基金联合资助
      作者简介:

      徐政语 男 1964年出生 博士 高级工程师 构造地质学与石油地质学 E-mail:Xuzy_hz@petrochina.com.cn

    • 中图分类号: P512.2;P595

    摘要: 为了深入探讨扬子陆块下古生界页岩发育与分布特征、建立沉积模式,系统收集与整理了扬子陆块下寒武统牛蹄塘组与上奥陶统—下志留统五峰—龙马溪组两套富有机质页岩大量数据,选取贵州省三都县渣拉沟及四川省筠连县昭104井两个典型剖面与井岩芯进行了系统观察与采样,对扬子陆块范围内两套富有机质页岩岩性与沉积相发育特征进行了系统分析.研究表明,早古生代以来,扬子陆块受被动大陆边缘扩张与陆缘造山挠曲坳陷两类成盆环境影响[1-2],牛蹄塘组页岩沉积于被动大陆边缘扩张环境,缘于上升洋流与缺氧事件复合沉积模式,富有机质页岩以扬子陆块东南缘深水陆棚—斜坡相区最为发育、厚度最大、有机碳含量最高;五峰—龙马溪组页岩沉积于加里东期周缘前陆造山环境,缘于浅水陆棚—闭塞滞留海湾沉积模式,富有机质页岩以中上扬子陆块东南缘深水陆棚区最为发育、厚度最大、有机碳含量最高.

    English Abstract

    徐政语, 蒋恕, 熊绍云, 梁兴, 王高成, 郭燕玲, 何勇, 饶大骞. 扬子陆块下古生界页岩发育特征与沉积模式[J]. 沉积学报, 2015, 33(1): 21-35. doi: 10.14027/j.cnki.cjxb.2015.01.003
    引用本文: 徐政语, 蒋恕, 熊绍云, 梁兴, 王高成, 郭燕玲, 何勇, 饶大骞. 扬子陆块下古生界页岩发育特征与沉积模式[J]. 沉积学报, 2015, 33(1): 21-35. doi: 10.14027/j.cnki.cjxb.2015.01.003
    XU ZhengYu, JIANG Shu, XIONG ShaoYun, LIANG Xing, WANG GaoCheng, GUO YanLing, HE Yong, RAO DaQian. Characteristics and Depositional Model of the Lower Paleozoic Organic Rich Shale in the Yangtze Continental Block[J]. Acta Sedimentologica Sinica, 2015, 33(1): 21-35. doi: 10.14027/j.cnki.cjxb.2015.01.003
    Citation: XU ZhengYu, JIANG Shu, XIONG ShaoYun, LIANG Xing, WANG GaoCheng, GUO YanLing, HE Yong, RAO DaQian. Characteristics and Depositional Model of the Lower Paleozoic Organic Rich Shale in the Yangtze Continental Block[J]. Acta Sedimentologica Sinica, 2015, 33(1): 21-35. doi: 10.14027/j.cnki.cjxb.2015.01.003
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