2015 Vol. 35, No. 3
Article Contents

YANG Chupeng, LI Xuejie, YAO Yongjian, CHANG Xiaohong, WU Jiaoqi, HUANG Lei, JU Dong. THE SUBSURFACE FLUID-FLOW SYSTEMS AND THEIR GENETIC MECHANISM IN THE SOUTHWESTERN BARENTS SEA[J]. Marine Geology & Quaternary Geology, 2015, 35(3): 135-144. doi: 10.3724/SP.J.1140.2015.03135
Citation: YANG Chupeng, LI Xuejie, YAO Yongjian, CHANG Xiaohong, WU Jiaoqi, HUANG Lei, JU Dong. THE SUBSURFACE FLUID-FLOW SYSTEMS AND THEIR GENETIC MECHANISM IN THE SOUTHWESTERN BARENTS SEA[J]. Marine Geology & Quaternary Geology, 2015, 35(3): 135-144. doi: 10.3724/SP.J.1140.2015.03135

THE SUBSURFACE FLUID-FLOW SYSTEMS AND THEIR GENETIC MECHANISM IN THE SOUTHWESTERN BARENTS SEA

  • The southwestern Barents Sea is a large hydrocarbon-prone epi-continental sea of the Eurasian Arctic region. Based on the large number of literatures on the hydrocarbon gas-flow in the southwestern Barents Sea, we summarized features of the gas-flow and discussed its genetic mechanism in this paper. The gas-flow features occurred in the area include pockmarks, gas chimneys, high amplitude anomalies (BSR), fluid leakage along faults and other fractures. And the occurrence of fluid-flow features suggests the direct relationship to the major deep-seated faults and their connection with hydrocarbon-bearing formations. The fluid flow is controlled by faults and matured source rocks. The close relation between fluid-flow features and structural elements indicates that extensional tectonics, uplift and glaciations could have played major roles in the formation of fluid leakage, although erosion might add some weight on it.
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  • [1] Dugan B, Flemings P B. Overpressure and fluid flow in the New Jersey continental slope:implications for slope failure and cold seeps[J]. Science, 2000, 289:288-291.

    Google Scholar

    [2] Doré A G, Jensen L N. The impact of late Cenozoic uplift and erosion on hydrocarbon exploration:offshore Norway and some other uplifted basins[J]. Global and Planetary Change, 1996, 12:415-436.

    Google Scholar

    [3] Mienert J, Bunz S, Guidard S, et al. Ocean bottom seismometer investigations in the Ormen Lange area offshore mid-Norway provide evidence for shallow gas layers in subsurface sediments[J]. Marine and Petroleum Geology, 2005, 22:287-297.

    Google Scholar

    [4] Cartwright J, Huuse M, Aplin A. Seal bypass systems[J]. AAPG Bulletin, 2007, 91:1141-1166.

    Google Scholar

    [5] Heggland R. Gas seepage as an indicator of deeper prospective reservoirs. A study based on exploration 3D seismic data[J]. Marine and Petroleum Geology, 1998, 15:1-9.

    Google Scholar

    [6] Perez-Garcia C, Feseker T, Mienert J, et al. The Håkon Mosby mud volcano:330000 years of focused fluid flow activity at the SW Barents Sea slope[J]. Marine Geology, 2009, 262:105-115.

    Google Scholar

    [7] Chand S, Rise L, Ottesen D, et al. Pockmark-like depressions near the Goliat hydrocarbon field, Barents Sea:morphology and genesis[J]. Marine and Petroleum Geology, 2009, 26:1035-1042.

    Google Scholar

    [8] Chand S, Thorsnes T, Rise L, et al. Multiple episodes of fluid flow in the SW Barents Sea (Loppa High) evidenced by gas flares, pockmarks and gas hydrate accumulation[J]. Earth and Planetary Science Letters, 2012, 331-332:305-314.

    Google Scholar

    [9] Ostanin I, Anka Z, di Primio R, et al. Identification of a large Upper Cretaceous polygonal fault network in the Hammerfest basin:implications on the reactivation of regional faulting and gas leakage dynamics, SW Barents Sea[J]. Marine Geology, 2012, 332-334:109-125.

    Google Scholar

    [10] Chand S, Mienert J, Andreassen K, et al. Gas hydrate stability zone modelling in areas of salt tectonics and pockmarks of the Barents Sea suggests an active hydrocarbon venting system[J]. Marine and Petroleum Geology, 2008, 25:625-636.

    Google Scholar

    [11] Heggland R. Definition of geohazards in exploration 3-D seismic data using attributes and neural-network analysis[J]. AAPG Bulletin, 2004, 88:857-868.

    Google Scholar

    [12] Meldahl P, Heggland R, Bril B, et al. Identifying faults and gas chimneys using multiattributes and neural networks[J]. The Leading Edge, 2001, 20:474-482.

    Google Scholar

    [13] Henriksen E, Ryseth A E, Larssen G B, et al. Tectonostratigraphy of the greater Barents Sea:implications for petroleum systems[J]. Arctic Petroleum Geology, 2011, Memoirs 35:163-195.

    Google Scholar

    [14] Vadakkepuliyambatta S, Bünz S, Mienert J, et al. Distribution of subsurface fluid-flow systems in the SW Barents Sea[J]. Marine and Petroleum Geology, 2013, 43:208-221.

    Google Scholar

    [15] Nickel J C, diPrimio R, Kallmeyer J, et al. Tracing the origin of thermogenic hydrocarbon signals in pockmarks from the southwestern Barents Sea[J]. Organic Geochemistry, 2013, 63:73-84.

    Google Scholar

    [16] Johansen S E, Ostisty B K, Birkeland Ø, et al. Hydrocarbon potential in the Barents Sea region:play distribution and potential[C]//Arctic Geology and Petroleum Potential. Elsevier, Amsterdam. 1993:273-320.

    Google Scholar

    [17] Gabrielsen R H, Faerseth R B, Jensen L N, et al. Structural elements of the Norwegian Continental Shelf, Part I:The Barents Sea Region[J]. NPD-Bulletin, 1990(6):1-33.

    Google Scholar

    [18] Faleide J I, Vågnes E, Gudlaugsson S T. Late Mesozoic-Cenozoic evolution of the south-western Barents Sea in a regional rift-shear tectonic setting[J]. Marine and Petroleum Geology, 1993, 10:186-214.

    Google Scholar

    [19] Eldholm O, Faleide J I, Myhre A M. Continent-ocean transition at the Western Barents Sea Svalbarrd continental-margin[J]. Geology, 1987, 15:1118-1122.

    Google Scholar

    [20] Solheim A, Kristoffersen Y. Sediments above the upper regional unconformity; thickness, seismic stratigraphy and outline of the glacial history[J]. Norsk Polar Institut Rapport serie, 1984, 179B:26.

    Google Scholar

    [21] Andreassen K, Nilssen E, Ødegaard C. Analysis of shallow gas and fluid migration within the Plio-Pleistocene sedimentary succession of the SW Barents Sea continental margin using 3D seismic data[J]. Geo-Marine Letters, 2007, 27:155-171.

    Google Scholar

    [22] Nickel J C, di Primio R, Mangelsdorf K, et al. Characterization of microbial activity in pockmark fields of the SW-Barents Sea[J]. Marine Geology, 2012, 332-334:152-162.

    Google Scholar

    [23] Doré A G. Barents Sea geology, petroleum resources and commercial potential[J]. Arctic, 1995, 48:207-221.

    Google Scholar

    [24] Bugge T, Elvebakk G, Fanavoll S, et al. Shallow stratigraphic drilling applied in hydrocarbon exploration of the Nordkapp Basin, Barents Sea[J]. Marine and Petroleum Geology, 2002, 19:13-37.

    Google Scholar

    [25] Larsen R M, Fjaeran T, Skarpnes O. Hydrocarbon potential of the Norwegian Barents Sea based on recent well results[C]//Arctic Geology and Petroleum Potential. Elsevier, Amsterdam, 1993:321-331.

    Google Scholar

    [26] Laberg J S, Andreassen K, Vorren T O. Late Cenozoic erosion of the high latitude southwestern Barents Sea shelf revisited[J]. Geological Society of America Bulletin, 2011, 124(1-2):77-88.

    Google Scholar

    [27] Connolly D L,Brouwer F, Walraven D. Detecting fault-related hydrocarbon migration pathways in seismic data:implications for fault-seal, pressure, and charge prediction[J]. Gulf Coast Association of Geological Societies Transactions, 2008, 58:191-203.

    Google Scholar

    [28] Løseth H, Gading M, Wensaas L. Hydrocarbon leakage interpreted on seismic data[J]. Marine and Petroleum Geology, 2009, 26:1304-1319.

    Google Scholar

    [29] Boitsov S, Petrova V, Jensen H K B, et al. Petroleum-related hydrocarbons in deep and subsurface sediments from south-western Barents Sea[J]. Marine Environmental Research, 2011, 71:357-368.

    Google Scholar

    [30] Fowler M G, Abolins P, Douglas A G. Monocyclic alkanes in Ordovician organic matter[J]. Organic Geochemistry, 1986, 10:815-823.

    Google Scholar

    [31] Ohm S E, Karlsen D A, Austin T J F. Geochemically driven exploration models in uplifted areas:examples from the Norwegian Barents Sea[J]. AAPG Bulletin, 2008, 92:1191-1223.

    Google Scholar

    [32] Talukder A R. Review of submarine cold seep plumbing systems:leakage to seepage and venting[J]. Terra Nova, 2012, 24:255-272.

    Google Scholar

    [33] Cavanagh A J, di Primio R, Scheck-Wenderoth M, et al. Severity and timing of Cenozoic exhumation in the southwestern Barents Sea[J]. Journal of the Geological Society, London, 2006,163:761-774.

    Google Scholar

    [34] Lerche I, Yu Z, Tørudbakken B, et al. Ice loading effects in sedimentary basins with reference to the Barents Sea[J]. Marine and Petroleum Geology, 1997, 14:277-338.

    Google Scholar

    [35] Ostanin I, Anka Z, di Primio R, et al. Hydrocarbon plumbing systems above the Snøhvit gas field:structural control and implications for thermogenic methane leakage in the Hammerfest Basin, SW Barents Sea[J]. Marine and Petroleum Geology, 2013, 43:127-146.

    Google Scholar

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