Abstract
Multichannel seismic (MCS) data from the Yaquina forearc basin off Peru reveal a complex distribution of gas and gas hydrate related reflections. Lateral variations of the reflection pattern at the assumed base of the gas hydrate stability zone in terms of continuity, amplitude, and signal attenuation underneath are observed, as well as the possible occurrence of paleo-bottom simulating reflectors (BSRs). Phase reversed reflections above the bottom simulating reflector point to free gas within the gas hydrate stability zone (GHSZ). To constrain the interpretation of the observed reflection pattern we calculated the velocity distribution along the MCS line from high-resolution ocean bottom hydrophone recordings with two independent methods. Heat flux values estimated on the basis of the velocity-depth functions increase with decreasing amplitude of the BSR and peak near chemoherms. These results suggest a model of the Yaquina Basin where free gas is trapped under parts of the BSR, and within the GHSZ, particularly under the seafloor and under an erosional unconformity. The hypothesis of a paleo-BSR that reflects the uplift of the base of the hydrate stability zone caused by the deposition of a particular sediment sequence is supported by the estimated heat flux values.
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References
Ballesteros MW, Moore GF, Taylor B, Ruppert S (1988) Seismic stratigraphic framework of the Lima and Yaquina forearc basins, Peru. In: Suess E, von Huene R (eds) Proceedings of ODP, initial reports 112. Ocean Drilling Program, College Station TX, pp 77–90
Bangs NL, Sawyer DS, Golovchenko X (1993) Free gas at the base of the gas hydrate zone in the vicinity of the Chile Tripple Junction. Geology 21:905–908
Bialas J, Kukowski N (2000) Peruvian cruise reports fresh insights into gas hydrates. First Break 18.8:360–362
Blair NE, Aller RC (1995) Anaerobic methane oxidation on the Amazon shelf. Geochim Cosmochim Acta 59:3707–3715
Boetius A, Suess E (2004) Hydrate Ridge: a natural laboratory for the study of microbial life fueled by methane from near-surface gas hydrates. Chem Geol 205:291–310. DOI:10.1016/j.chemgeo.2003.12.034
Bourgois J,von Huene R, Pautot G, Huchon P (1988) Jean Charcot Seabeam survey along ODP Leg 112 northern transect. In: Suess E, von Huene R (eds) Proceedings of ODP, initial reports 112. Ocean Drilling Program, College Station, pp 131–137
Foucher JP, Nouzé H, Henry P (2002) Observation of a double BSR on the Nakai slope. Mar Geol 187:161–175
Gorman AR, Holbrook WS, Hornbach M, Hackwith KL, Lizarralde D, Pecher IA (2002) Migration of methane gas through the hydrate stability zone in a low-flux hydrate province. Geology 30:327–330
Grevemeyer L, Villinger H (2001) Gas hydrate stability and the assessment of heat flow through continental margins. Geophys J Int 145:647–660
Hampel A (2002) The migration history of the Nazca Ridge along the Peruvian active margin: a re-evaluation. Earth Planet Sci Lett 203:665–679
Helgerud MB, Dvorkin J, Nur A, Sakai A, Collett T (1999) Elastic-wave velocity in marine sediments with gas hydrates: effective medium modeling. Geophys Res Lett 26(13):2021–2024
Hempel P, Spiess V, Schreiber R (1994) Expulsion of shallow gas in the Skagerrak—evidence from sub-bottom profiling, seismic, hydroacoustical and geochemical data. Estuarine Coastal Shelf Sci 38:583–601
Holbrook WS, Hoskins H, Wood WT, Stephen RA, Lizarralde D, The Leg 164 Shipboard Scientific Party (1996) Methane hydrate and free gas on the Blake Ridge from vertical seismic profiling. Science 273:1840–1843
Holbrook WS, Gorman AR, Hornbach MJ, Hackwith KL, Nealon J, Lizarralde D, Pecher IA (2002) Seismic detection of marine methane hydrate. Leading Edge 21/7:686–689
Hornbach MJ, Holbrook WS, Gorman AR, Hackwith KL, Lizarralde D, Pecher IA (2003) Direct seismic detection of methane hydrate on the Blake Ridge. Geophysics 68/1:92–100. DOI: 10.1190/1.1543196
Hübscher CP, Kukowski N (2003) Complex BSR Pattern in the Yaquina Basin off Peru: implications for impact of anisotropic permeability and tectonic. Geol Mar Lett 23/2:91–101. DOI: 10.1007/s00367-003-0128-z
von Huene R, Pecher IA (1999) Neotectonics and the origins of BSRs along the Peru margin. Earth Planet Sci Lett 166:47–55
Katzman R, Holbrook WS, Paull CK (1994) Combined vertical-incidence and wide-angle seismic study of a gas hydrate zone, Blake Ridge. J Geophys Res 99:17975–17995
Kaul N, Rosenberger A, Villinger H (2000) Comparison of measured and BSR-derived heat flow values, Makran accretionary prism, Pakistan. Mar Geol 164:37–51
Korenaga J, Holbrook WS, Singh SC, Minshull TA (1997) Natural gas hydrates on the southeast US Margin: constraints from full waveform inversion and traveltime inversions of wide-angle seismic data. J Geophys Res 99:9681–9695
Kvenvolden KA (1998) A primer on the geological occurrence of gas hydrate. In: Henriet JP, Mienert J (eds) Gas hydrates: relevance to world margin stability and climate change. Geol Soc Spec Pub 137, London, pp 9–30
Kvenvolden KA, Kastner M (1990) Gas hydrates of the Peruvian outer continental margin. In: Suess E, von Huene R (eds) Proceedings of ODP, scientific results 112. Ocean Drilling Program, College Station, pp 517–526
Lee W, Hutchinson DR, Collett TS, Dillon WP (1996) Seismic velocities for hydrate-bearing sediments using weighted equation. J Geophys Res 101:20347–20358
Lodolo E, Camerlenghi A, Madrussani G, Tinivella U, Rossi G (2002) Assessment of gas hydrate and free gas distribution on the South Shetland margin (Antarctica) based on multichannel seismic reflection data. Geophys J Int 148:103–119
Lüdmann T, Wong HK (2003) Characteristics of gas hydrate occurrences associated with mud diapirism and gas escape structures in the northwestern Sea of Okhotsk. Mar Geol 201:269–286. DOI: 10.1016/S0025-3227(03)00224-X
MacKay ME, Jarrard RD, Westbrook GK, Hyndman RD (1994) Origin of bottom simulating reflectors: geophysical evidence from the Cascadia accretionary prism. Geology 22:459–462
Mienert J, Posewang J (1999) Evidence of shallow- and deep-water gas hydrate destabilizations in North Atlantic polar continental margin sediments. Geol Mar Lett 19:143–149
Milkov VA, Dickens GR, Claypool GE, Lee Yj, Borowski WS, Torres ME, Xu W, Tomaru H, Tréhu AM, Schultheiss P (2004) Co-existence of gas hydrate, free gas, and brine within the regional gas hydrate stability zone at Hydrate Ridge (Oregon margi): evidence from prolonged degassing of a pressurized core. Earth Planet Sci Lett 222:829–843. DOI:10.1016/jepsl.2004.03.028
Miller JJ, Lee MW, von Huene R (1991) An analysis of a seismic reflection from a base of a gas hydrate zone, offshore Peru. Am Assoc Petrol Geol Bull 75(5):910–924
Minshull TA, Singh SC, Westbrook GK (1994) Seismic velocity structure at a gas hydrate reflector, offshore western Colombia, from full waveform inversion. J Geophys Res 99:4715–4734
Moore GF, Taylor B (1988) Structure of the Peru forearc from multichannel seismic reflection data. In: Suess E, von Huene R (eds) Proceedings of ODP, initial reports 112. Ocean Drilling Program, College Station, pp 71–76
Pecher IA (1995) Seismic studies of bottom simulating reflectors at the convergent margins offshore Peru and Costa Rica. PhD Thesis, University of Kiel. GEOMAR report 47:159
Pecher IA, Minshull TA, Singh SC, von Huene R (1996) Free gas at a bottom simulating reflector off Peru: results from full waveform inversion. Earth Planet Sci Lett 139:459–469
Pecher IA, Kukowski N, Hübscher C, Greinert P, Bialas J, GEOPECO Working Group (2001) The link between bottom-simulating reflections and methane flux into the gas hydrate stability zone—new evidence from Lima Basin, Peru Margin. Earth Planet Sci Lett 185:343–354
Posewang J, Mienert J (1999a) High-resolution seismic studies of gas hydrates west of Svalbard. Geol Mar Lett 19:150–156
Posewang J, Mienert J (1999b) The enigma of double BSRs: indicators for changes in the hydrate stability field. Geol Mar Lett 19:157–163
Rowe MM, Gettrust JF (1993) Fine structure of methane hydrate-bearing sediments on the Blake outer ridge as determined from deep-tow multichannel seismic data. J Geophys Res 98:463–473
Shipboard Scientific Party (1988a) Proceedings of ODP, initial reports 112. Ocean Drilling Program, College Station
Shipboard Scientific Party (1988b) Site 685. In: Suess E, von Huene R et al (eds) Proceedings of ODP, initial reports 112, College Station, pp 597–704
Shipboard Scientific Party (2002) In: Proceedings of ODP, initial reports 204, Ocean Drilling Program, College Station
Shipley TH, Houston M, Buffler R (1979) Seismic reflection evidence for the widespread occurrence of possible gas hydrate horizons on continental slopes and rises. Am Assoc Petrol Geol Bull 63:2204–2213
Singh SC, Minshull TA, Spence GD (1993) Velocity structure of a gas hydrate reflector. Science 260:204–207
Sloan ED (1990) Clathrate hydrates of natural gases. Marcel Bekker Inc, New York, p 641
Sloan ED Jr (1998) Physical/chemical properties of gas hydrates and applications to world margin stability and climate change. In: Henriet JP, Mienert J (eds) Gas hydrates: relevance to world margin stability and climate change. Geol Soc Spec Pub 137, London, pp 31–50
Suess E, Torres ME, Bohrmann G, Collier RW, Greinert J, Linke P, Rehter G, Trehu AM, Wallmann K, Winckler G, Zulegger E (1999) Gas hydrate destabilization: enhanced dewatering, benthic material turnover, and large methane plumes at the Cascadia convergent margin. Earth Planet Sci Lett 170:1–15
Suess E, Torres ME, Bohrmann G, Collier RW, Rickert D, Goldfinger C, Linke P, Heuser A, Sahling H, Heeschen K, Jung C, Nakamura K, Greinert J, Pfannkuche O, Trehu A, Klinkhammer G, Whiticar MJ, Eisenhauer A, Teichert B, Elvert M (2001) Sea floor methane hydrates at Hydrate Ridge, Cascadia margin. In: Paull CK, Dillon WP (eds) Natural gas hydrates: occurrence, distribution, and detection. Am Geophys Union, Geophys Monogr Ser 124, pp 87–98
Torres ME, Colbert S, Collier RW, deAngelis M, Hammond D, Heeschen K, Hubbard D, McManus J, Moyer C, Rehder G, Trehu AM, Tyron M, Whaling P (1998) Active gas discharge resulting from decomposition of gas hydrates on Hydrate Ridge, Cascadia margin. Eos Trans 79:461
Whalley E (1980) Speed of longitudinal sound in clathrate hydrates. J Geophys Res 85:2539–2542
Wood WT, Stoffa PL, Shipley TH (1994) Quantitative detection of methane hydrate through high-resolution seismic velocity analysis. J Geophys Res 99:9681–9695
Yamano M, Uyeda S (1990) Heat flow studies in the Peru subduction zone. In: Proceedings of ODP, scientific results 112, Ocean Drilling Program, College Station, pp 653–661
Yamano M, Uyeda S, Aoki Y, Shipley TH (1982) Estimates of heat flow derived from gas hydrates. Geology 10:339–343
Zelt CA, Smith RB (1992) Seismic traveltime inversion for 2-D crustal velocity structure. Geophys J Int 8:16–34
Acknowledgements
We would like to thank Dirk Kläschen for the initial geometry processing of OBH recording. Thanks to Nina Kukowski and Ingo Pecher for fruitful discussions. Special thanks to Tim Minshull for his comments on this manuscript. We also want to thank Ingo Pecher and Kirk McIntosh, the manuscript was greatly improved by their reviews. Further, we are grateful to Captain H. Papenhagen and his crew for the excellent support onboard RV Sonne. The GEOPECO project was funded by BMBF grant 03G0146B/0. Additional funding was supplied by the Marie Curie Training Site at Southampton Oceanography Centre.
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Netzeband, G.L., Hübscher, C.P., Gajewski, D. et al. Seismic velocities from the Yaquina forearc basin off Peru: evidence for free gas within the gas hydrate stability zone. Int J Earth Sci (Geol Rundsch) 94, 420–432 (2005). https://doi.org/10.1007/s00531-005-0483-2
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DOI: https://doi.org/10.1007/s00531-005-0483-2