CSCD来源期刊

北大中文核心期刊

中国科技核心期刊

地学领域高质量科技期刊分级T2区（2023）

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Volume 43 Issue 4
Jul.  2024
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Article Contents
Article Navigation >  Bulletin of Geological Science and Technology  > 2024  >  43(4): 167-180
YI Yuhao, BAO Hanyong, ZHU Hongtao, LU Yaqiu, MENG Zhiyong, LI Kai, CHEN Fayao. Radiolarian assemblage from the Upper Permian Wujiaping Formation in the eastern Sichuan Basin and its hydrocarbon source significance[J]. Bulletin of Geological Science and Technology, 2024, 43(4): 167-180. doi: 10.19509/j.cnki.dzkq.tb20230721
Citation: YI Yuhao, BAO Hanyong, ZHU Hongtao, LU Yaqiu, MENG Zhiyong, LI Kai, CHEN Fayao. Radiolarian assemblage from the Upper Permian Wujiaping Formation in the eastern Sichuan Basin and its hydrocarbon source significance[J]. Bulletin of Geological Science and Technology, 2024, 43(4): 167-180. doi: 10.19509/j.cnki.dzkq.tb20230721
shu

Radiolarian assemblage from the Upper Permian Wujiaping Formation in the eastern Sichuan Basin and its hydrocarbon source significance

doi: 10.19509/j.cnki.dzkq.tb20230721
  • 1.

    Exploration and Development Research Institute, SINOPEC Jianghan Oilfield Company, Wuhan 430223, China

  • 2a.

    School of Earth Resources, China University of Geosciences (Wuhan), Wuhan 430074, China

  • 2b.

    School of Earth Sciences, China University of Geosciences (Wuhan), Wuhan 430074, China

More Information
  • Corresponding author: YI Yuhao, E-mail: cugyyh@163.com
  • Received Date: 29 Dec 2023
  • Accepted Date: 22 Apr 2024
  • Rev Recd Date: 25 Feb 2024
    Abstract
  • Objective

    The upper Permian Wujiaping Formation in the Hongxing area of eastern Sichuan Province has good shale gas accumulation conditions and is also an important successor for Permian shale gas exploration in the Sichuan Basin. However, the formation mechanism of these siliceous-argillaceous source rocks is still unclear. Apart from their petromineralogical characteristics, geochemical composition and macrofossil assemblage (represented by radiolarian) are also important for identifying the genesis of this siliceous-argillaceous source rock.

    Methods

    Radiolarian is a significant planktonic component of the Phanerozoic marine ecosystem. Various radiolarian assemblages indicate different sedimentary environments, and their abundance is a good indicator of palaeoproductivity. In this study, radiolarians were separated by the acid-etching method to identify different morphological characteristics, and the correlation between radiolarian abundance and total organic carbon (TOC) content was also analysed through thin-section observation.

    Results

    A large number of radiolarians were found in the Wujiaping Formation in the Well HY3 in the Hongxing area of eastern Sichuan Province. These fossils were identified as Spumellaria and Entactinaria, belonging to a typical shallow-water radiolarian assemblage, namely, the Se assemblage. In the Second Member of the Wujiaping Formation, the radiolarian abundance exhibited a relatively positive correlation with the TOC content.

    Conclusion

    Based on the radiolarian assemblage characteristics, sedimentary sequence and palaeogeographic background of the Wujiaping Formation, it is inferred that these source rocks from the Second Member of the Wujiaping Formation formed in a shallow-water environment less than 60 m deep. The accumulation of organic matter in the Second Member of the Wujiaping Formation was probably affected by primary productivity, redox conditions, terrigenous debris input and upwelling, among which high palaeoproductivity was one of the main controlling factors.

     

    • The authors declare that no competing interests exist.
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  • [1]
    ARTHUR A M. Marine black shales: Depositional mechanisms and environments of ancient deposits[J]. Annual Review of Earth and Planetary Sciences, 1994, 22: 499-551. doi: 10.1146/annurev.ea.22.050194.002435
    [2]
    TYSON R V. The "productivity versus preservation" controversy: Cause, flaws and resolution[C]//HARRIS N B. The Deposition of Organic-Carbon-Rich Sediments: Models, Mechanisms, and Consequences. [S. l]: SEPM(Society for Sedimentary Geology), 2005, 82: 17-33.
    [3]
    PEDERSEN T F, CALVERT S E. Anoxia vs. productivity: What controls the formation of organic-carbon-rich and sedimentary rocks[J]? The American Association of Petroleum Geologists Bulletin, 1990, 74(4): 454-466.
    [4]
    TYSON R V, PEARSON T H. Modern and ancient continental shelf anoxia: An overview[J]. Geological Society, London, Special Publications, 1991, 58(1): 1-24. doi: 10.1144/GSL.SP.1991.058.01.01
    [5]
    DEMAISON G J, MOORE G T. Anoxic environments and oil source bed genesis[J]. Organic Geochemistry, 1980, 2(1): 9-31. doi: 10.1016/0146-6380(80)90017-0
    [6]
    HUANG S P, JIANG Q C, JIANG H, et al. Genetic and source differences of gases in the Middle Permian Qixia and Maokou formations in the Sichuan Basin, SW China[J]. Organic Geochemistry, 2023, 178: 104574. doi: 10.1016/j.orggeochem.2023.104574
    [7]
    蔡勋育, 韦宝东, 赵培荣. 南方海相烃源岩特征分析[J]. 天然气工业, 2005, 25(3): 20-22. https://www.cnki.com.cn/Article/CJFDTOTAL-TRQG200503006.htm

    CAI X Y, WEI B D, ZHAO P R. Characteristics of the marine hydrocarbon source rocks in South China[J]. Natural Gas Industry, 2005, 25(3): 20-22. (in Chinese with English abstract) https://www.cnki.com.cn/Article/CJFDTOTAL-TRQG200503006.htm
    [8]
    金之钧, 郑和荣, 蔡立国, 等. 中国前中生代海相烃源岩发育的构造-沉积条件[J]. 沉积学报, 2010, 28(5): 875-883. https://www.cnki.com.cn/Article/CJFDTOTAL-CJXB201005006.htm

    JIN Z J, ZHENG H R, CAI L G, et al. Tectonic-sedimentary conditions for development of Pre-Mesozoic marine source rocks in China[J]. Acta Sedimentologica Sinica, 2010, 28(5): 875-883. (in Chinese with English abstract) https://www.cnki.com.cn/Article/CJFDTOTAL-CJXB201005006.htm
    [9]
    张金川, 史淼, 王东升, 等. 中国页岩气勘探领域和发展方向[J]. 天然气工业, 2021, 41(8): 69-80. https://www.cnki.com.cn/Article/CJFDTOTAL-TRQG202108011.htm

    ZHANG J C, SHI M, WANG D S, et al. Fields and directions for shale gas exploration in China[J]. Natural Gas Industry, 2021, 41(8): 69-80. (in Chinese with English abstract) https://www.cnki.com.cn/Article/CJFDTOTAL-TRQG202108011.htm
    [10]
    WU W, LIU W Q, MOU C L, et al. Organic-rich siliceous rocks in the Upper Permian Dalong Formation (NW Middle Yangtze): Provenance, paleoclimate and paleoenvironment[J]. Marine and Petroleum Geology, 2021, 123: 104728. doi: 10.1016/j.marpetgeo.2020.104728
    [11]
    ZHANG B L, YAO S P, WIGNALL P B, et al. Widespread coastal upwelling along the Eastern Paleo-Tethys Margin (South China) during the Middle Permian (Guadalupian): Implications for organic matter accumulation[J]. Marine and Petroleum Geology, 2018, 97: 113-126. doi: 10.1016/j.marpetgeo.2018.06.025
    [12]
    ZHANG B L, YAO S P, HU W X, et al. Middle Permian palaeoclimatic-palaeoceanographic evolution and its controls on organic matter accumulation in the Lower Yangtze upwelling region[J]. International Journal of Coal Geology, 2022, 264: 104132. doi: 10.1016/j.coal.2022.104132
    [13]
    CHEN C, MU C L, ZHOU K K, et al. The geochemical characteristics and factors controlling the organic matter accumulation of the Late Ordovician-Early Silurian marine black shale in the Upper Yangtze Basin, South China[J]. Marine and Petroleum Geology, 2016, 76: 159-175. doi: 10.1016/j.marpetgeo.2016.04.022
    [14]
    LI Y F, ZHANG T W, ELLIS G S, et al. Depositional environment and organic matter accumulation of Upper Ordovician-Lower Silurian marine shale in the Upper Yangtze Platform, South China[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2017, 466: 252-264. doi: 10.1016/j.palaeo.2016.11.037
    [15]
    ZHANG K X, LI X S, WANG Y X, et al. Paleo-environments and organic matter enrichment in the shales of the Cambrian Niutitang and Wunitang fomrations, South China: Constraints from depositional environments and geochemistry[J]. Marine and Petroleum Geology, 2021, 134: 105329. doi: 10.1016/j.marpetgeo.2021.105329
    [16]
    ZHOU L, KANG Z H, WANG Z X, et al. Sedimentary geochemical investigation for paleoenvironment of the Lower Cambrian Niutitang Formation shales in the Yangtze Platform[J]. Journal of Petroleum Science and Engineering, 2017, 159: 376-386. doi: 10.1016/j.petrol.2017.09.047
    [17]
    包汉勇, 赵帅, 梁榜, 等. 川东红星地区二叠系吴家坪组页岩气富集高产主控因素与勘探启示[J]. 中国石油勘探, 2023, 28(1): 71-82. https://www.cnki.com.cn/Article/CJFDTOTAL-KTSY202301007.htm

    BAO H Y, ZHAO S, LIANG B, et al. Enrichment and high yield of shale gas in the Permian Wujiaping Formation in Hongxing area of eastern Sichuan and its exploration implications[J]. China Petroleum Exploration, 2023, 28(1): 71-82. (in Chinese with English abstract) https://www.cnki.com.cn/Article/CJFDTOTAL-KTSY202301007.htm
    [18]
    宋腾, 李世臻, 张焱林, 等. 鄂西地区上二叠统海相页岩气富集条件差异与控制因素: 以红星区块吴家坪组二段和恩施地区大隆组为例[J]. 天然气地球科学, 2023, 34(8): 1425-1441. https://www.cnki.com.cn/Article/CJFDTOTAL-TDKX202308009.htm

    SONG T, LI S Z, ZHANG Y L, et al. Gas differential enrichment characteristics and controlling factors of Upper Permian marine shale in western Hubei area: Case study of Wujiaping Formation Ⅱ in Hongxing Block and Dalong Formation in Enshi area[J]. Natural Gas Geoscience, 2023, 34(8): 1425-1441. (in Chinese with English abstract) https://www.cnki.com.cn/Article/CJFDTOTAL-TDKX202308009.htm
    [19]
    王必金, 包汉勇, 刘皓天, 等. 川东红星地区吴家坪组富有机质页岩特征与发育控制因素[J]. 地质科技通报, 2023, 42(5): 70-81. doi: 10.19509/j.cnki.dzkq.tb20230149

    WANG B J, BAO H Y, LIU H T, et al. Characteristics and controlling factors of the organic-rich shale in the Wujiaping Formation of the Hongxing area, eastern Sichuan Basin[J]. Bulletin of Geological Science and Technology, 2023, 42(5): 70-81. (in Chinese with English abstract) doi: 10.19509/j.cnki.dzkq.tb20230149
    [20]
    郑爱维, 孟志勇, 李凯, 等. 川东红星地区二叠系吴家坪组页岩储层纵向非均质性特征及其发育主控因素[J]. 天然气地球科学, 2023, 34(9): 1500-1514. https://www.cnki.com.cn/Article/CJFDTOTAL-TDKX202309003.htm

    ZHENG A W, MENG Z Y, LI K, et al. Vertical heterogeneity characteristics and main controlling factors of the Permian Wujiaping Formation shale reservoir in Hongxing area, eastern Sichuan[J]. Natural Gas Geoscience, 2023, 34(9): 1500-1514. (in Chinese with English abstract) https://www.cnki.com.cn/Article/CJFDTOTAL-TDKX202309003.htm
    [21]
    LIN L B, YU Y, GAO J, et al. The origin and geochemical characteristics of Permian chert in the Eastern Sichuan Basin, China[J]. Carbonates and Evaporites, 2018, 33: 613-624. doi: 10.1007/s13146-017-0372-3
    [22]
    YU Y, LIN L B, DENG X L, et al. Geochemical features of the Middle-Upper Permian cherts and implications for origin, depositional environment in the Sichuan Basin, SW China[J]. Geological Journal, 2020, 55(2): 1493-1506. doi: 10.1002/gj.3511
    [23]
    LUO J X, HE Y B, WANG R, et al. Lithofacies palaeogeography of the Late Permian Wujiaping Age in the Middle and Upper Yangtze region, China[J]. Journal of Palaeogeography, 2014, 3(4): 384-409.
    [24]
    曹涛涛, 邓模, 刘光祥, 等. 鄂西利川地区二叠系吴家坪组富有机质硅质页岩储层特征[J]. 海相油气地质, 2018, 23(3): 32-42. https://www.cnki.com.cn/Article/CJFDTOTAL-HXYQ201803004.htm

    CAO T T, DENG M, LIU G X, et al. Reservoir characteristics of organic-rich siliceous shale of Permian Wujiaping Formation in Lichuan area, western Hubei Province[J]. Marine Origin Petroleum Geology, 2018, 23(3): 32-42. (in Chinese with English abstract) https://www.cnki.com.cn/Article/CJFDTOTAL-HXYQ201803004.htm
    [25]
    翟常博, 牟传龙, 梁薇, 等. 鄂西地区二叠系孤峰组-大隆组沉积演化及其页岩气地质意义[J]. 矿物岩石, 2021, 41(4): 114-124. https://www.cnki.com.cn/Article/CJFDTOTAL-KWYS202104011.htm

    ZHAI C B, MOU C L, LIANG W, et al. Sedimentary evolution characteristics of Permian Gufeng Formation-Dalong Formation in western Hubei Province and its geological significance for the geological survey of shale gas[J]. Mineralogy and Petrology, 2021, 41(4): 114-124. (in Chinese with English abstract) https://www.cnki.com.cn/Article/CJFDTOTAL-KWYS202104011.htm
    [26]
    马恺, 张兵, 王艳, 等. 四川盆地高峰场地区上二叠统吴家坪组页岩石英成因研究[J]. 矿物岩石, 2022, 42(3): 67-77. https://www.cnki.com.cn/Article/CJFDTOTAL-KWYS202203007.htm

    MA K, ZHANG B, WANG Y, et al. Study on the genesis of different lithfacies quartz in Wujiaping Formation shale in Gaofengchang area, Sichuan Basin[J]. Mineralogy and Petrology, 2022, , 42(3): 67-77. (in Chinese with English abstract) https://www.cnki.com.cn/Article/CJFDTOTAL-KWYS202203007.htm
    [27]
    王一刚, 文应初, 洪海涛, 等. 四川盆地及邻区上二叠统-下三叠统海槽的深水沉积特征[J]. 石油与天然气地质, 2006, 27(5): 702-714. https://www.cnki.com.cn/Article/CJFDTOTAL-SYYT200605022.htm

    WANG Y G, WEN Y C, HONG H T, et al. Petroleum geological characteristics of deep water deposits in Upper Permian-Lower Triassic trough in Sichuan Basin and adjacent areas[J]. Oil & Gas Geology, 2006, 27(5): 702-714. (in Chinese with English abstract) https://www.cnki.com.cn/Article/CJFDTOTAL-SYYT200605022.htm
    [28]
    卓皆文, 王剑, 汪正江, 等. 鄂西地区晚二叠世沉积特征与台内裂陷槽的演化[J]. 新疆石油地质, 2009, 30(3): 300-303. https://www.cnki.com.cn/Article/CJFDTOTAL-XJSD200903011.htm

    ZHUO J W, WANG J, WANG Z J, et al. Sedimentary characteristics of Late Permian in western Hubei Province and evolution of inter-platform rift[J]. Xinjiang Petroleum Geology, 2009, 30(3): 300-303. (in Chinese with English abstract) https://www.cnki.com.cn/Article/CJFDTOTAL-XJSD200903011.htm
    [29]
    KAMETAKA M, TAKEBE, M, NAGAI H, et al. Sedimentary environments of the Middle Permian phosphorite-chert complex from the northeastern Yangtze Platform, China; the Gufeng Formation: A continental shelf radiolarian chert[J]. Sedimentary Geology, 2005, 174(3/4): 197-222.
    [30]
    MURCHEY B L, JONES D L. A Mid-Permian chert event: Widespread deposition of biogenic siliceous sediments in coastal, island arc and oceanic basins[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 1992, 96(1/2): 161-174.
    [31]
    ZHANG B L, CAO J, MU L, et al. The Permian chert event in South China: New geochemical constraints and global implications[J]. Earth-Science Reviews, 2023, 244: 104513.
    [32]
    DEMASTER D J. The supply and accumulation of silica in the marine environment[J]. Geochimica et Cosmochimica Acta, 1981, 45(10): 1715-1732.
    [33]
    HARPER H E, KNOLL A H. Silica, diatoms, and Cenozoic radiolarian evolution[J]. Geology, 1975, 3(4): 175-177.
    [34]
    BOLTOVSKOY D. Classification and distribution of South Atlantic Recent polycystine Radiolaria[J]. Palaeontologia Electronica, 1998: 1.2.6 A.
    [35]
    CASEY R E, WIGLEY C R, PEREZ-GUZMÁN A M. Biogeographic and ecologic perspective on polycystine radiolarian evolution[J]. Paleobiology, 1983, 9(4): 363-376.
    [36]
    ITAKI T. Depth-related radiolarian assemblage in the water-column and surface sediments of the Japan Sea[J]. Marine Micropaleontology, 2003, 47(3/4): 253-270.
    [37]
    FENG Q L, ALGEO T J. Evolution of oceanic redox conditions during the Permo-Triassic transition: Evidence from deep water radiolarian facies[J]. Earth-Science Reviews, 2014, 137: 34-51.
    [38]
    XIAO Y F, SUZUKI N, HE W H. Water depths of the Latest Permian (Changhsingian) radiolarians estimated from correspondence analysis[J]. Earth-Science Reviews, 2017, 173: 141-158.
    [39]
    CARON D A, MICHAELS A F, SWANBERG N R, et al. Primary productivity by symbiont-bearing planktonic sarcodines (Acantharia, Radiolaria, Foraminifera) in surface waters near Bermuda[J]. Journal of Plankton Research, 1995, 17(1): 103-129.
    [40]
    DENNETT M R, CARON D A, MICHAELS A F, et al. Video plankton recorder reveals high abundances of colonial Radiolaria in surface waters of the central North Pacific[J]. Journal of Plankton Research, 2002, 24(8): 797-805.
    [41]
    CAULET J P, VÉNEC-PEYRÉ M T, VERGNAUD-GRAZZINI C, et al. Variation of South Somalian upwelling during the last 160 ka: Radiolarian and foraminifera records in core MD 85674[J]. Upwelling System: Evolution Since the Early Miocene, Geological Society, London, Special Publications, 1992, 64(1): 379-389.
    [42]
    JIN Y X, NOBLE P J, POULSON S R. Paleoenvironmental and paleoecological implications of Permian (Guadalupian) radiolarian and geochemical variations in the Lamar Limestone, Delaware Basin, West Texas (USA)[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2012, 346: 37-53.
    [43]
    LAZARUS D, BITTNIOK B, DIESTER-HAASS L, et al. Comparison of radiolarian and sedimentologic paleoproductivity proxies in the Latest Miocene-Recent Benguela Upwelling System[J]. Marine Micropaleontology, 2006, 60(4): 269-294.
    [44]
    SHI L, FENG Q L, SHEN J, et al. Proliferation of shallow-water radiolarians coinciding with enhanced oceanic productivity in reducing conditions during the Middle Permian, South China: Evidence from the Gufeng Formation of western Hubei Province[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2016, 444: 1-14.
    [45]
    刘宝珺, 许效松. 中国南方岩相古地理图集[M]. 北京: 科学出版社, 1994: 133-138.

    LIU B J, XU X S. Lithofacies paleogeography atlas of South China[M]. Beijing: Science Press, 1994: 134-138. (in Chinese)
    [46]
    沈树忠, 张华, 张以春, 等. 中国二叠纪综合地层和时间框架[J]. 中国科学(地球科学), 2019, 49(1): 160-193. https://www.cnki.com.cn/Article/CJFDTOTAL-JDXK201901009.htm

    SHEN S Z, ZHANG H, ZHANG Y C, et al. Permian integrative stratigraphy and timescale of China[J]. Science China (Earth Sciences), 2019, 49(1): 160-193. (in Chinese with English abstract) https://www.cnki.com.cn/Article/CJFDTOTAL-JDXK201901009.htm
    [47]
    HE B, XU Y G, GUAN, J P, et al. Paleokarst on the top of the Maokou Formation: Further evidence for domal crustal uplift prior to the Emeishan flood volcanism[J]. Lithos, 2010, 119(1/2): 1-9.
    [48]
    杨宝忠, 张宁, 夏文臣. 重庆石柱地区上二叠统吴家坪阶牙形石动物群及沉积环境[J]. 地质科技情报, 2008, 27(4): 27-32. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ200804006.htm

    YANG B Z, ZHANG N, XIA W C. Conodont fauna and sedimentary environment of Wuchiapingian of Upper Permian in Shizhu area, Chongqing[J]. Geological Science and Technology Information, 2008, 27(4): 27-32. (in Chinese with English abstract) https://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ200804006.htm
    [49]
    ZHANG L L, ZHANG N, XIA W C. Conodont succession in the Guadalupian-Lopingian boundary interval of the Maoershan section, Hubei Province, China[J]. Micropaleontology, 2007, 53(6): 433-446.
    [50]
    李泯星, 屈海洲, 曾琪, 等. 四川盆地西北部上二叠统吴家坪组火山碎屑岩孔隙演化特征及有利储集区分布[J]. 天然气地球科学, 2020, 31(11): 1574-1584. https://www.cnki.com.cn/Article/CJFDTOTAL-TDKX202011006.htm

    LI M X, QU H Z, ZENG Q, et al. Pore evolution characteristics and distribution of favorable reservoir area of the Upper Permian Wujiaping Formation in the northwestern Sichuan[J]. Natural Gas Geoscience, 2020, 31(11): 1574-1584. (in Chinese with English abstract) https://www.cnki.com.cn/Article/CJFDTOTAL-TDKX202011006.htm
    [51]
    曾琪, 胡欣, 屈海洲, 等. 川西北部地区上二叠统吴家坪组的地层划分及有利储集岩分布[J]. 天然气勘探与开发, 2020, 43(4): 33-47. https://www.cnki.com.cn/Article/CJFDTOTAL-TRKT202004005.htm

    ZENG Q, HU X, QU H Z, et al. Division of strata and distribution of favorable reservoir rocks of the Upper Permian Wujiaping Formation in the northwestern Sichuan Basin[J]. Natural Gas Exploration and Development, 2020, 43(4): 33-47. (in Chinese with English abstract) https://www.cnki.com.cn/Article/CJFDTOTAL-TRKT202004005.htm
    [52]
    易雨昊, 朱红涛, 陆亚秋, 等. 川东红星地区上二叠统吴家坪组沉积相演化与核形石发育条件[J/OL]. 地球科学: 1-22[2024-03-14]. https://link.cnki.net/urlid/42.1874.P.20240313.1618.004.html.

    YI Y H, ZHU H T, LU Y Q, et al. Sedimentary facies evolution and oncoidal development conditions of the Wujiaping Formation of Upper Permian in Hongxing area[J]. Earth Science: 1-22[2024-03-14]. https://link.cnki.net/urlid/42.1874.P.20240313.1618.004
    [53]
    FENG Q L, HE W H, GU S Z, et al. Latest Permian Spumellaria and Entactinaria (radiolaria) from South China[J]. Revue de Micropaléontologie, 2006, 49(1): 21-43.
    [54]
    杜永灯, 沈俊, 冯庆来. 放射虫在生产力和烃源岩研究中的应用[J]. 地球科学, 2012, 37(增刊2): 147-155. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX2012S2021.htm

    DU Y D, SHEN J, FENG Q L. Applications of radiolarian for productivity and hydrocarbon-source rocks[J]. Earth Science, 2012, 37(S2): 147-155. (in Chinese with English abstract) https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX2012S2021.htm
    [55]
    何卫红. 煤山D剖面的放射虫动物群与海平面变化[J]. 地球科学(中国地质大学学报), 2006, 31(2): 159-164. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200602002.htm

    HE W H. Changhsingian radiolarian fauna from the Meishan D section and sea-level changes[J]. Earth Science (Journal of China University of Geosciences), 2006, 31(2): 159-164. (in Chinese with English abstract) https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200602002.htm
    [56]
    向宇, 冯庆来, 沈俊, 等. 贵州安顺长兴阶放射虫动物群及其与TOC和古生产力的关系[J]. 中国科学(地球科学), 2013, 43: 1047-1056. https://www.cnki.com.cn/Article/CJFDTOTAL-JDXK201306013.htm

    XIANG Y, FENG Q L, SHEN J, et al. Changhsingian radiolarian fauna from Anshun, Guizhou, and its relationship to TOC and paleo-productivity[J]. Science China (Earth Sciences), 2013, 43: 1047-1056. (in Chinese with English abstract) https://www.cnki.com.cn/Article/CJFDTOTAL-JDXK201306013.htm
    [57]
    HE W H, FENG Q L, GU S Z, et al. Changxingian(Upper Permian) radiolarian fauna from Meishan D Section, Changxing, Zhejiang, China, and its possible paleoecological significance[J]. Journal of Paleontology, 2005, 79(2): 209-218.
    [58]
    聂小妹, 雷勇, 冯庆来, 等. 四川广元上寺剖面长兴阶放射虫动物群演变及控制因素[J]. 地质论评, 2012, 58(5): 809-815. https://www.cnki.com.cn/Article/CJFDTOTAL-DZLP201205003.htm

    NIE X M, LEI Y, FENG Q L, et al. Evolution and its control factors of the Changshingian radiolarian fauna at the Shangsi Section in Jiange County, Guangyuan City, Sichuan Province[J]. Geological Review, 2012, 58(5): 809-815. (in Chinese with English abstract) https://www.cnki.com.cn/Article/CJFDTOTAL-DZLP201205003.htm
    [59]
    GUI B W, FENG Q L, YUAN A H. Late Changhsingian (Latest Permian) radiolarians from Chaohu, Anhui[J]. Journal of Earth Science, 2009, 20(5): 797-810.
    [60]
    马强分, 冯庆来. 湖北建始罗家坝剖面孤峰组放射虫分类及地层研究[J]. 微体古生物学报, 2012, 29(4): 402-415. https://www.cnki.com.cn/Article/CJFDTOTAL-WSGT201204009.htm

    MA Q F, FENG Q L. Taxonomy and biostratigraphy of the Middle Permian radiolarian fauna from the Gufeng Formation in Luojiaba, West Hubei Province[J]. Acta Micropalaeontologica Sinica, 2012, 29(4): 402-415. (in Chinese with English abstract) https://www.cnki.com.cn/Article/CJFDTOTAL-WSGT201204009.htm
    [61]
    FENG Q L, HE W H, GU S Z, et al. Radiolarian evolution during the Latest Permian in South China[J]. Global and Planetary Change, 2007, 55: 177-192.
    [62]
    胡明毅, 魏欢, 邱小松, 等. 鄂西利川见天坝长兴组生物礁内部构成及成礁模式[J]. 沉积学报, 2012, 30(1): 33-42. https://www.cnki.com.cn/Article/CJFDTOTAL-CJXB201201004.htm

    HU M Y, WEI H, QIU X S, et al. Reef composition and their forming models of Changxing Formation in Jiantianba Section of Lichuan, western Hubei[J]. Acta Sedimentologica Sinica, 2012, 30(1): 33-42. (in Chinese with English abstract) https://www.cnki.com.cn/Article/CJFDTOTAL-CJXB201201004.htm
    [63]
    王延奇, 胡明毅, 刘富艳, 等. 鄂西利川见天坝长兴组海绵礁岩石类型及礁体演化阶段[J]. 岩性油气藏, 2008, 20(3): 44-48. https://www.cnki.com.cn/Article/CJFDTOTAL-YANX200803013.htm

    WANG Y Q, HU M Y, LIU F Y, et al. Rock types and evolution of reef of Changxing Formation in Jiantianba of western Hubei[J]. Lithologic Reservoirs, 2008, 20(3): 44-48. (in Chinese with English abstract) https://www.cnki.com.cn/Article/CJFDTOTAL-YANX200803013.htm
    [64]
    TOURTELOT H H. Black shale: Its deposition and diagenesis[J]. Clays and Clay Minerals, 1979, 27(5): 313-321.
    [65]
    陈木宏, 黄良民, 涂霞, 等. 南海放射虫与初级生产力的古海洋学转换关系[J]. 科学通报, 1999, 44(3): 327-333. https://www.cnki.com.cn/Article/CJFDTOTAL-KXTB199903022.htm

    CHEN M H, HUANG L M, TU X, et al. Paleoceanographic transition relationship between radiolaria and primary productivity in the South China Sea[J]. Chinese Science Bulletin, 1999, 44(3): 327-333. (in Chinese) https://www.cnki.com.cn/Article/CJFDTOTAL-KXTB199903022.htm
    [66]
    吴勘. 扬子北缘中二叠统孤峰组地球生物学构成及页岩气地质特征[D]. 武汉: 中国地质大学(武汉), 2013.

    WU K. Geobiological composition and geological characters of shale gas from the Middle Permian Gufeng Formation in the north margin of Yangtze[D]. Wuhan: China University of Geosciences (Wuhan), 2013. (in Chinese with English abstract)
    [67]
    腾格尔, 秦建中, 付小东, 等. 川东北地区上二叠统吴家坪组烃源岩评价[J]. 古地理学报, 2010, 12(3): 334-345. https://www.cnki.com.cn/Article/CJFDTOTAL-GDLX201003012.htm

    TENG G R, QIN J Z, FU X D, et al. Hydrocarbon source rocks evaluation of the Upper Permian Wujiaping Formation in northeastern Sichuan area[J]. Journal of Palaeogeography, 2010, 12(3): 334-345. (in Chinese with English abstract) https://www.cnki.com.cn/Article/CJFDTOTAL-GDLX201003012.htm
    [68]
    韦恒叶, 胡谍, 邱振, 等. 川北-鄂西上二叠统富有机岩沉积与地球化学特征[J/OL]. 沉积学报: 1-34[2023-10-07]. https://link.cnki.net/urlid/62.1038.P.20231007.1217.001.html.

    WEI H Y, HU D, QIU Z, et al. Sedimentological and geochemical characteristics of Late Permian organic-rich rocks in North Sichuan and West Hubei Province[J/OL]. Acta Sedimentologica Sinica: 1-34[2023-10-07]. https://link.cnki.net/urlid/62.1038.P.20231007.1217.001.html.
    [69]
    杨雨, 汪华, 谢继容, 等. 页岩气勘探新领域: 四川盆地开江-梁平海槽二叠系海相页岩气勘探突破及展望[J]. 天然气工业, 2023, 43(11): 19-27. https://www.cnki.com.cn/Article/CJFDTOTAL-TRQG202311003.htm

    YANG Y, WANG H, XIE J R, et al. Exploration breakthrough and prospect of Permian marine shale gas in the Kaijiang-Liangping trough, Sichuan Basin[J]. Natural Gas Industry, 2023, 43(11): 19-27. (in Chinese with English abstract) https://www.cnki.com.cn/Article/CJFDTOTAL-TRQG202311003.htm
    [70]
    DIESTER-HAASS L. Radiolarian/planktonic foraminiferal ratios in a coastal upwelling region[J]. Journal of Foraminiferal Research, 1977, 7(1): 26-33.
    [71]
    TRÉGUER J P, DE LA ROCHA L C. The world ocean silica cycle[J]. Annual Review of Earth and Planetary Sciences, 2013, 5: 477-501.
    [72]
    李艳芳, 邵德勇, 吕海刚, 等. 四川盆地五峰组-龙马溪组海相页岩元素地球化学特征与有机质富集的关系[J]. 石油学报, 2015, 36(12): 1470-1483. https://www.cnki.com.cn/Article/CJFDTOTAL-SYXB201512002.htm

    LI Y F, SHAO D Y, LÜ H G, et al. A relationship between elemental geochemical characteristics and organic matter enrichment in marine shale of Wufeng Formation-Longmaxi Formation, Sichuan Basin[J]. Acta Petrolei Sinica, 2015, 36(12): 1470-1483. (in Chinese with English abstract) https://www.cnki.com.cn/Article/CJFDTOTAL-SYXB201512002.htm
    [73]
    王超, 张柏桥, 舒志国, 等. 焦石坝地区五峰组-龙马溪组页岩纹层发育特征及其储集意义[J]. 地球科学, 2019, 44(3): 972-982. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX201903024.htm

    WANG C, ZHANG B Q, SHU Z G, et al. Shale lamination and its influence on shale reservoir quality of Wufeng Formation-Longmaxi Formation in Jiaoshiba area[J]. Earth Science, 2019, 44(3): 972-982. (in Chinese with English abstract) https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX201903024.htm
    [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, 2014, 41(1): 28-36. https://www.cnki.com.cn/Article/CJFDTOTAL-SKYK201401003.htm

    GUO T L, ZHANG H R. Formation and enrichment mode of Jiaoshiba shale gas field, Sichuan Basin[J]. Petroleum Exploration and Development, 2014, 41(1): 28-36. (in Chinese with English abstract) https://www.cnki.com.cn/Article/CJFDTOTAL-SKYK201401003.htm
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