Muzhuang YANG, Yun HE. Gas hydrate system and resource potential of the continental margin of the Bellingshausen Sea to the west coast of the Antarctic Peninsula[J]. Marine Geology & Quaternary Geology, 2019, 39(4): 136-147. DOI: 10.16562/j.cnki.0256-1492.2018111202
Citation: Muzhuang YANG, Yun HE. Gas hydrate system and resource potential of the continental margin of the Bellingshausen Sea to the west coast of the Antarctic Peninsula[J]. Marine Geology & Quaternary Geology, 2019, 39(4): 136-147. DOI: 10.16562/j.cnki.0256-1492.2018111202

Gas hydrate system and resource potential of the continental margin of the Bellingshausen Sea to the west coast of the Antarctic Peninsula

More Information
  • Received Date: November 11, 2018
  • Revised Date: March 20, 2019
  • Based on the geological environment of the continental margin of the Bellinsgauzen Sea and the presence of natural gas hydrate proxies, such as BSR and the rapid accumulation of sediments from the upper reaches, it is inferred that the region has excellent conditions for natural gas hydrate accumulation. According to the drilling data and seismic profiles of the Leg 178 of the ODP Pacific Drilling Program, formation conditions of natural gas hydrates in the study area are analyzed according to sedimentation, gas source, heat flow field and key time of accumulation. The accumulation conditions of natural gas hydrates are predicted by the comprehensive anomaly map and the comprehensive accumulation system table of the study area. It is predicted that the gas hydrate accumulation area along the sea margin off the Antarctic Peninsula is mainly located on the continental rise of Drift 7, most probably in the stratigraphic units Ⅰ and Ⅱ, from Holocene to late Pliocene (0~2.1 Ma). Volumetric method is used to calculate the amount of natural gas hydrate resources, which are very large. The results may provide a good reference to the future investigation and research of natural gas hydrates in the Antarctic region.
  • [1]
    Kvenvolden K A. Methane hydrate-A major reservoir of carbon in the shallow geosphere[J]. Chemical Geology, 1988, 71(1-3);41-51. doi: 10.1016/0009-2541(88)90104-0
    [2]
    吴庐山, 邓希光, 梁金强, 等.南极陆缘天然气水合物特征及资源前景[J].海洋地质与第四纪地质, 2010, 30(1):95-107. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=hydzydsjdz201001014

    WU Lushan, DENG Xiguang, LIANG Jinqiang, et al.The characteristics and resource potential of gas hydrates in the antarcmargins[J].Marine Geology & Quaternary Geology, 2010, 30(1):95-107. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=hydzydsjdz201001014
    [3]
    Herron E M, Tucholke B E. Sea-floor magnetic patterns and basement structure in the southeastern Pacific[J]. Initial Rep. Deep Sea Drill. Proj, 1976, 35: 263-278.
    [4]
    Lodolo E, Camerlenghi A, Brancolini G. A bottom simulating reflector on the South Shetland Margin, Antarctic Peninsula[J]. Antarctic Science, 1993, 2(5):207-210. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=S0954102093000264
    [5]
    何韵, 杨木壮.南极半岛别林斯高晋海天然气水合物成矿条件与成矿机理[J].海洋地质前沿, 2018, 34(4):16-24. http://d.old.wanfangdata.com.cn/Periodical/hydzdt201804003

    HE Yun, YANG Muzhuang.Forming conditions and mechanism of gas hydrates in the Bellinsgauzen sea, Antarctic Peninsula[J].Marine Geology Frontiers, 2018, 34(4):16-24. http://d.old.wanfangdata.com.cn/Periodical/hydzdt201804003
    [6]
    Barker P F. The Cenozoic subduction history of the Pacific margin of the Antarctic Peninsula: ridge crest-trench interactions[J]. Journal of the Geological Society, 1982, 139(6): 787-801. doi: 10.1144/gsjgs.139.6.0787
    [7]
    Larter R D, Rebesco M, Vanneste L E, et al. Cenozoic tectonic, sedimentary and glacial history of the continental shelf west of Graham Land, Antarctic Peninsula[M]. American Geophysical Union, 1997.
    [8]
    Rebesco M, Larter R D, Barker P F, et al. The history of sedimentation on the continental rise west of the Antarctic Peninsula[M]. American Geophysical Union, 1997.
    [9]
    Larter R, Rebesco M, Vanneste L E, et al. Seismic reflection investigations on the Pacific margin of the Antarctic Peninsula[J]. Terra Antartica, 1994, 1(2): 271-274.
    [10]
    Rebesco M L R D C. Giant sediment drifts on the continental rise west of the Antarctic Peninsula[J]. Geo-Marine Letters, 1996, 16(2):65-75. doi: 10.1007/BF02202600
    [11]
    Rebesco M, Camerlenghi A, Zanolla C. Bathymetry and morphogenesis of the continental margin west of the Antarctic Peninsula[J]. Terra Antart, 1998, 5(4): 715-725.
    [12]
    Diviacco P, Rebesco M, Camerlenghi A. Late Pliocene mega debris flow deposit and related fluid escapes identified on the Antarctic Peninsula continental margin by seismic reflection data analysis[J]. Marine Geophysical Researches, 2006, 27(2): 109-128. doi: 10.1007/s11001-005-3136-8
    [13]
    Diviacco P, Wardell N. Reprocessing and dissemination of Antarctic Seismic Data[J]. Terra Antarctica, 2003, 9: 133-136.
    [14]
    Shipboard Scientific Party. Site 1096[C]//Barker P F, Camerlenghi A, Acton G D, et al. Proceedings of the Ocean Drilling Program, Initial Reports Volume 178: College Station TX (Ocean Drilling Program). 1999.
    [15]
    Venuti A, Florindo F, Caburlotto A, et al. Late Quaternary sediments from deep-sea sediment drifts on the Antarctic Peninsula Pacific margin: Climatic control on provenance of minerals[J]. Journal of Geophysical Research Solid Earth, 2011, 116(B6).
    [16]
    Andrew T, Che-Chuan Lin, Char-Shine Liu, et al. Gas-hydrate Petroleum Systems, Play Types and Prospects in an Accretionary Wedge and its Adjacent Rifted Continental Margin, Taiwan[C]// Proceedings of the 7th International Conference on Gas Hydrates (ICGH 2011).Edinburgh, Scotland, United Kingdom, 2011.
    [17]
    Michael Max, Arthur Johnson. Hydrate petroleum system approach to natural gas hydrate exploration[C]//Proceedings of the 7th International Conference on Gas Hydrates (ICGH 2011).Edinburgh, Scotland, United Kingdom, 2011.
    [18]
    Larter R D, Barker P F. Effects of ridge crest-trench interaction on Antarctic-Phoenix spreading: forces on a young subducting plate[J]. Journal of Geophysical Research: Solid Earth, 1991, 96(B12): 19583-19607. doi: 10.1029/91JB02053
    [19]
    Cunningham A P, Larter R D, Barker P F, et al. Tectonic evolution of the Pacific margin of Antarctica 2. Structure of Late Cretaceous-early Tertiary plate boundaries in the Bellingshausen Sea from seismic reflection and gravity data[J]. Journal of Geophysical Research, 2002, 107(B12):EPM-1-EPM 6-20.
    [20]
    Dowdeswell J A, Cofaigh C ó, Noormets R, et al. A major trough-mouth fan on the continental margin of the Bellingshausen Sea, West Antarctica: the Belgica Fan[J]. Marine Geology, 2008, 252(3-4): 129-140. doi: 10.1016/j.margeo.2008.03.017
    [21]
    Larter R D, Rebesco M, Vanneste L E, et al. Cenozoic tectonic, sedimentary and glacial history of the continental shelf west of Graham Land, Antarctic Peninsula[J]. Geology and Seismic Stratigraphy of the Antarctic Margin, 1997, 2: 1-27.
    [22]
    Tomlinson J S, Pudsey C J, Livermore R A, et al. Long-range sidescan sonar (GLORIA) survey of the Antarctic Peninsula Pacific margin[C]//Yoshida Y, Kaminuma K, Shiraishi K (Eds.). Recent Progress in Antarctic Earth Science. Proceedings 6th International Symposium Antarctic Earth Science.Tokyo, 1992: 423-429.
    [23]
    McGinnis J P, Hayes D E, Driscoll N W. Sedimentary processes across the continental rise of the southern Antarctic Peninsula[J]. Marine Geology, 1997, 141(1-4): 91-109. doi: 10.1016/S0025-3227(97)00056-X
    [24]
    Anderson J B, Wellner J S, Lowe A L, et al. Footprint of the Expanded West Antarctic Ice Sheet: Ice Stream History and Behavior[J]. Gsa Today, 2001, 11(10): 4-9. doi: 10.1130/1052-5173(2001)011<0004:FOTEWA>2.0.CO;2
    [25]
    Rebesco M, Pudsey C J, Canals M, et al. Sediment drifts and deep-sea channel systems, Antarctic Peninsula Pacific Margin[J]. Geological Society London Memoirs, 2002, 22(1):353-371. doi: 10.1144/GSL.MEM.2002.022.01.25
    [26]
    Dowdeswell J A, Cofaigh C ó, Pudsey C J. Continental slope morphology and sedimentary processes at the mouth of an Antarctic palaeo-ice stream[J]. Marine Geology, 2004, 204(1-2): 203-214. doi: 10.1016/S0025-3227(03)00338-4
    [27]
    Scheuer C, Gohl K, Larter R D, et al. Variability in Cenozoic sedimentation along the continental rise of the Bellingshausen Sea, West Antarctica[J]. Marine Geology, 2006, 227(3-4): 279-298. doi: 10.1016/j.margeo.2005.12.007
    [28]
    Noormets R, Dowdeswell J A, Larter R D, et al. Morphology of the upper continental slope in the Bellingshausen and Amundsen Seas-Implications for sedimentary processes at the shelf edge of West Antarctica[J]. Marine Geology, 2009, 258(1-4): 100-114. doi: 10.1016/j.margeo.2008.11.011
    [29]
    Sloan Jr E D. Clathrate Hydrates of Natural Gases, Revised and Expanded[M]. CRC Press, 1998.
    [30]
    金春爽, 汪集旸, 王永新, 等.天然气水合物地热场分布特征[J].地质科学, 2004, 39(3): 416-423. doi: 10.3321/j.issn:0563-5020.2004.03.011

    JIN Chunshuang, WANG Jiyang, WANG Yongxin, et al.Geothermal field characteristics in the areas of gas hydrates distribution [J].Chinese Journal of Geology, 2004, 39(3): 416-423. doi: 10.3321/j.issn:0563-5020.2004.03.011
    [31]
    Diviacco P, Rebesco M, Camerlenghi A. Late Pliocene mega debris flow deposit and related fluid escapes identified on the Antarctic Peninsula continental margin by seismic reflection data analysis[J]. Marine Geophysical Researches, 2006, 27(2): 109-128. doi: 10.1007/s11001-005-3136-8
    [32]
    梁金强, 吴能友, 杨木壮, 等.天然气水合物资源量估算方法及应用[J].地质通报, 2006, 25(9): 1205-1210. doi: 10.3969/j.issn.1671-2552.2006.09.038

    LIANG Jinqiang, WU Nengyou, YANG Muzhuang, et al. Resource estimate method of gas hydrates and its application[J].Geological Bulletin of China, 2006, 25(9): 1205-1210. doi: 10.3969/j.issn.1671-2552.2006.09.038
  • Cited by

    Periodical cited type(1)

    1. 康玉柱. 中国南海地块天然气水合物成藏条件探讨. 油气藏评价与开发. 2021(05): 659-668 .

    Other cited types(0)

Catalog

    Article views (3218) PDF downloads (39) Cited by(1)

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return