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Fluid venting and seepage at accretionary ridges: the Four Way Closure Ridge offshore SW Taiwan

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Abstract

Within the accretionary prism offshore SW Taiwan, widespread gas hydrate accumulations are postulated to occur based on the presence of a bottom simulating reflection. Methane seepage, however, is also widespread at accretionary ridges offshore SW Taiwan and may indicate a significant loss of methane bypassing the gas hydrate system. Four Way Closure Ridge, located in 1,500 m water depth, is an anticlinal ridge that would constitute an ideal trap for methane and consequently represents a site with good potential for gas hydrate accumulations. The analysis of high-resolution bathymetry, deep-towed sidescan sonar imagery, high-resolution seismic profiling and towed video observations of the seafloor shows that Four Way Closure Ridge is and has been a site of intensive methane seepage. Continuous seepage is mainly evidenced by large accumulations of authigenic carbonate precipitates, which appear to be controlled by the creation of fluid pathways through faulting. Consequently, Four Way Closure Ridge is not a closed system in terms of fluid migration and seepage. A conceptual model of the evolution of gas hydrates and seepage at accretionary ridges suggests that seepage is common and may be a standard feature during the geological development of ridges in accretionary prisms. The observation of seafloor seepage alone is therefore not a reliable indicator of exploitable gas hydrate accumulations at depth.

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References

  • Berndt C (ed) (2013) RV SONNE Fahrtbericht/Cruise Report SO227 TAIFLUX: Fluid and gas migration in the transition from a passive to an active continental margin off SW Taiwan, 02.04. - 02.05.2013, Kaohsiung - Kaohsiung (Taiwan). GEOMAR Report NS 011, 104 p. doi:10.3289/GEOMAR_REP_NS_11_2013

  • Bowin C, Lu RS, Lee CS, Schouten H (1978) Plate convergence und accretion in the Taiwan-Luzon region. AAPG Bull 62:1645–1672

    Google Scholar 

  • Bünz S, Mienert J (2004) Acoustic imaging of gas hydrate and free gas at the Storegga Slide. J Geophys Res 109, B04102. doi:10.1029/2003JB002863

    Article  Google Scholar 

  • Bünz S, Mienert J, Berndt C (2003) Geological controls on the Storegga gas-hydrate system of the mid-Norwegian continental margin. Earth Planet Sci Lett 209:291–307

    Article  Google Scholar 

  • Carson B, Seke E, Paskevich V, Holmes ML (1994) Fluid expulsion sites on the Cascadia accretionary prism: mapping diagenetic deposits with processed GLORIA imagery. J Geophys Res Solid Earth 99:11959–11969

    Article  Google Scholar 

  • Chen SC, Hsu SK, Tsai CH, Ku CY, Yeh YC, Wang Y (2010) Gas seepage, pockmarks and mud volcanoes in the near shore of SW Taiwan. Mar Geophys Res 31:133–147

    Article  Google Scholar 

  • Chen L, Chi WC, Wu SK, Liu CS, Shyu CT, Wang Y, Lu CY (2014) Two-dimensional fluid flow models at two gas hydrate sites offshore south-western Taiwan. J Asian Earth Sci 92:245–253

    Article  Google Scholar 

  • Chi WC, Reed D, Liu CS, Lundberg N (1998) Distribution of the bottom-simulating reflector in the offshore Taiwan collision zone. Terr Atmos Ocean Sci 9:779–794

    Google Scholar 

  • Chiu JK, Tseng WH, Liu CS (2006) Distribution of gassy sediments and mud volcanoes offshore southwestern Taiwan. Terr Atmos Ocean Sci 17:703–722

    Google Scholar 

  • Chuang PC, Yang TF, Hong WL, Lin S, Sun CH, Lin AT, Chen JC, Wang Y, Chung SH (2010) Estimation of methane flux offshore SW Taiwan and the influence of tectonics on gas hydrate accumulation. Geofluids 10:497–510

    Article  Google Scholar 

  • Conti S, Artoni A, Piola G (2007) Seep-carbonates in a thrust-related anticline at the leading edge of an orogenic wedge: the case of the middle late Miocene Salsomaggiore Ridge (northern Apennines, Italy). Sediment Geol 199:233–251

    Article  Google Scholar 

  • Crutchley GJ, Geiger S, Pecher IA, Gorman AR, Zhu H, Henrys SA (2010) The potential influence of shallow gas and gas hydrates on sea floor erosion of Rock Garden, an uplifted ridge offshore of New Zealand. Geo-Mar Lett 30:283–303

    Article  Google Scholar 

  • Crutchley GJ, Berndt C, Geiger S, Klaeschen D, Papenberg C, Klaucke I, Hornbach MJ, Bangs NLB, Maier C (2013) Drivers of focused fluid flow and methane seepage at south Hydrate Ridge, offshore Oregon, USA. Geology 41:551–554

    Article  Google Scholar 

  • Eakin DH, McIntosh KD, Van Avendonk HJA, Lavier L, Lester R, Lee CS (2014) Crustal-scale seismic profiles across the Manila subduction zone: the transition from intra-oceanic subduction to incipient collision. J Geophys Res Solid Earth 119:1–17

    Article  Google Scholar 

  • Fuh SC, Liu CS, Lundberg N, Reed D (1997) Strike-slip faults offshore southern Taiwan: implications for the oblique arc-continent collision processes. Tectonophysics 274:25–39

    Article  Google Scholar 

  • Hornbach MJ, Saffer DM, Holbrook WS (2004) Critically pressured free-gas reservoirs below gas-hydrate provinces. Nature 427:142–144

    Article  Google Scholar 

  • Hsiung KH, Yu HS (2011) Morpho-sedimentary evidence for a canyon-channel-trench interconnection along the Taiwan-Luzon plate margin, South China Sea. Geo-Mar Lett 31:215–226

    Article  Google Scholar 

  • Hyndman RD, Foucher JP, Yamamo M, Fisher A, Shipboard Scientific Party ODP Leg 131 (1992) Deep sea bottom-simulating-reflectors: calibration of the base of the hydrate stability field as used for heat flow estimates. Earth Planet Sci Lett 109:289–301

    Article  Google Scholar 

  • Jin YK, Kim YG, Baranov B, Shoji H, Obzhirov A (2011) Distribution and expression of gas seeps in a gas hydrate province of the northeastern Sakhalin continental slope, Sea of Okhotsk. Mar Pet Geol 28:1844–1855

    Article  Google Scholar 

  • Johnson JE, Goldfinger C, Suess E (2003) Geophysical constraints on the surface distribution of authigenic carbonates across the Hydrate Ridge region, Cascadia margin. Mar Geol 202:79–120

    Article  Google Scholar 

  • Kawamoto T (2013) The first offshore MH production test. http://energy.gov/sites/prod/files/2013/06/f1/Takami%20Kawamoto%20-%20The%20First%20Offshore%20Production%20Test.pdf. Accessed 20 Mar 2015

  • Klaucke I, Masson DG, Petersen CJ, Weinrebe W, Ranero CR (2008) Multifrequency geoacoustic imaging of fluid escape structures offshore Costa Rica: implications for the quantification of seep processes. Geochem Geophys Geosyst 9, Q04010. doi:10.1029/2007GC001708

    Article  Google Scholar 

  • Klaucke I, Weinrebe RW, Petersen CJ, Bowen DA (2010) Temporal variability of gas seeps offshore New Zealand: multi-frequency geoacoustic imaging of the Wairarapa area Hikurangi margin. Mar Geol 272:49–58

    Article  Google Scholar 

  • Kroeger KF, Plaza-Faverola A, Barnes PM, Pecher IA (2015) Thermal evolution of the New Zealand Hikurangi subduction margin: impact on natural gas generation and methane hydrate formation - a model study. Mar Pet Geol 63:97–114

    Article  Google Scholar 

  • Le Bas TP, Huvenne VAI (2009) Acquisition and processing of backscatter data for habitat mapping: comparison of multibeam and sidescan systems. Appl Acoust 70:1248–1257

    Article  Google Scholar 

  • Lin AT, Yao B, Hsu SK, Liu CS, Huang CY (2009) Tectonic features of the incipient arc-continent collision zone of Taiwan: implications for seismicity. Tectonophysics 479:28–42

    Article  Google Scholar 

  • Lin CC, Lin AT, Liu CS, Horng CS, Chen GY, Wand Y (2014) Canyon-infilling and gas hydrate occurrences in the frontal fold of the offshore accretionary wedge off southern Taiwan. Mar Geophys Res 35:21–35

    Article  Google Scholar 

  • Liu CS, Deffontaines B, Lu CY, Lallemand S (2004) Deformation patterns of an accretionary wedge in the transition zone from subduction to collision offshore southwestern Taiwan. Mar Geophys Res 25:123–137

    Article  Google Scholar 

  • Liu CS, Schnürle P, Wang Y, Chung SH, Chen SC, Hsiuan TH (2006) Distribution and characters of gas hydrate offshore of southwestern Taiwan. Terr Atmos Ocean Sci 17:615–644

    Google Scholar 

  • Moore JC, Vrolijk P (1992) Fluids in accretionary prisms. Rev Geophys 30:113–135

    Article  Google Scholar 

  • Park JO, Tsuru T, Kodaira S, Cummins PR, Kaneda Y (2002) Splay fault branching along the Nankai subduction zone. Science 297:1157–1160

    Article  Google Scholar 

  • Reed DL, Lundberg N, Liu CS, Kuo BY (1992) Structural relations along the margins of the offshore Taiwan accretionary wedge: implications for accretion and crustal kinematics. Acta Geol Taiwan 30:105–122

    Google Scholar 

  • Saffer DM, Tobin HJ (2011) Hydrology and mechanics of subduction zone forearcs: fluid flow and pore pressure. Annu Rev Earth Planet Sci 39:157–186

    Article  Google Scholar 

  • Schnürle P, Liu CS, Lin AT, Lin S (2011) Structural controls on the formation of BSR over a diapiric anticline from a MCS survey offshore southwestern Taiwan. Mar Pet Geol 28:1932–1942

    Article  Google Scholar 

  • Shipley TH, Houston MH, Buffler RT, Shaub FJ, McMillen KJ, Ladd JW, Worzel JL (1979) Seismic evidence for widespread possible gas hydrate horizons on continental slopes and rises. AAPG Bull 63:2204–2213

    Google Scholar 

  • Taylor B, Hayes DE (1983) Origin und history of the South China Sea basin. AGU Geophys Monogr 27:23–56

    Google Scholar 

  • Tréhu AM, Flueh ER (2001) Estimating the thickness of the free gas zone beneath Hydrate Ridge, Oregon continental margin, from seismic velocities and attenuation. J Geophys Res 106:2035–2045

    Article  Google Scholar 

  • Tréhu AM, Flemings PB, Bangs NL, Chevallier J, Gracia E, Johnson JE, Liu CS, Liu X, Riedel M, Torres ME (2004a) Feeding methane vents and gas hydrate deposits at south Hydrate Ridge. Geophys Res Lett 31, L23310. doi:10.1029/2004GL021286

    Article  Google Scholar 

  • Tréhu AM, Long PE, Torres ME, Bohrmann G, Rack FR, Collett TS, Goldberg DS, Milkov AV, Riedel M, Schultheiss P, Bangs NL, Barr SR, Borowski WS, Claypool GE, Delwiche ME, Dickens GR, Gracia E, Guérin G, Holland M, Johnson JE, Lee YJ, Liu CS, Su X, Teichert B, Tomaru H, Vanneste M, Watanabe M, Weinberger JL (2004b) Three-dimensional distribution of gas hydrate beneath southern Hydrate Ridge: constraints from ODP Leg 204. Earth Planet Sci Lett 222:845–862

    Article  Google Scholar 

  • Tsuji Y, Namikawa T, Fujii T, Hayashi M, Kitamura R, Nakamizu M, Ohbi K, Saeki T, Yamamoto K, Inamori T, Oikawa N, Shimizu S, Kawasaki M, Nagakubo S, Matsushima J, Ochiai K, Okui T (2009) Methane-hydrate occurrence and distribution in the eastern Nankai Trough, Japan: findings of the Tokai-oki to Kumano-nada methane-hydrate drilling program. In: Collett T, Johnson A, Knapp C, Boswell R (eds) Natural gas hydrates—Energy resource potential and associated geologic hazards. AAPG Memoir 89:228–246

  • Weinberger JL, Brown KM (2006) Fracture networks and hydrate distribution at Hydrate Ridge, Oregon. Earth Planet Sci Lett 245:123–136

    Article  Google Scholar 

  • Westbrook GK, Chand S, Rossi G, Long C, Bünz S, Camerlenghi A, Carcione JM, Dean S, Foucher JP, Flueh ER, Gei D, Haacke RR, Madrussani G, Mienert J, Minshull TA, Nouzé H, Peacock S, Reston TJ, Vanneste M, Zillmer M (2008) Estimation of gas hydrate concentration from multi-component seismic data at sites on the continental margins of NW Svalbard and the Storegga region of Norway. Mar Pet Geol 25:744–758

    Article  Google Scholar 

  • Yang TF, Chuang PC, Lin S, Chen JC, Wang Y, Chung SH (2006) Methane venting in gas hydrate potential area offshore of SW Taiwan: evidence of gas analysis of water column samples. Terr Atmos Ocean Sci 17:933–950

    Google Scholar 

  • Yu HS, Chang JF (2002) The Penghu submarine canyon off southwestern Taiwan: morphology and origin. Terrest Atmos Ocean Sci 13:547–562

  • Zwart G, Moore JC, Cochrane GR (1996) Variations in temperature gradients identify active faults in the Oregon accretionary prism. Earth Planet Sci Lett 139:485–495

    Article  Google Scholar 

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Acknowledgements

Captain Meyer and his crew are thanked for the excellent support during RV SONNE cruise SO227. Financial support by the German Ministry of Education and Research (BmBF grant 03G0227A) and Taiwan’s National Energy Program is acknowledged. Comments by W. Sager, A. Tréhu and the editors proved useful in improving the article.

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Authors and Affiliations

  1. GEOMAR Helmholtz-Centre for Ocean Research Kiel, Wischhofstr. 1-3, 24148, Kiel, Germany

    Ingo Klaucke, Christian Berndt & Sina Muff

  2. GNS Science, P.O. Box 30-368, Lower Hutt, 5040, New Zealand

    Gareth Crutchley

  3. Institute of Earth Sciences, Academia Sinica, Taipei, Taiwan, ROC

    Wu-Cheng Chi

  4. Institute of Oceanography, National Taiwan University, Roosevelt Road, Taipei, Taiwan, ROC

    Saulwood Lin

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  1. Ingo Klaucke
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  2. Christian Berndt
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  4. Wu-Cheng Chi
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  5. Saulwood Lin
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  6. Sina Muff
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Correspondence to Ingo Klaucke.

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Responsible guest editor: M. De Batist

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Klaucke, I., Berndt, C., Crutchley, G. et al. Fluid venting and seepage at accretionary ridges: the Four Way Closure Ridge offshore SW Taiwan. Geo-Mar Lett 36, 165–174 (2016). https://doi.org/10.1007/s00367-015-0431-5

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  • DOI: https://doi.org/10.1007/s00367-015-0431-5

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