High-resolution resistivity imaging of marine gas hydrate structures by combined inversion of CSEM towed and ocean-bottom receiver data

被引:38
作者
Attias, Eric [1 ,5 ]
Weitemeyer, Karen [1 ,6 ]
Hoelz, Sebastian [2 ]
Naif, Samer [3 ]
Minshull, Tim A. [1 ]
Best, Angus I. [4 ]
Haroon, Amir [2 ]
Jegen-Kulcsar, Marion [2 ]
Berndt, Christian [2 ]
机构
[1] Univ Southampton, Natl Oceanog Ctr Southampton, Ocean & Earth Sci, Southampton SO14 3ZH, Hants, England
[2] GEOMAR Helmholtz Ctr Ocean Res, Marine Geodynam, D-24148 Kiel, Germany
[3] Columbia Univ, Lamont Doherty Earth Observ, Palisades, NY 10964 USA
[4] Univ Southampton, Natl Oceanog Ctr, Waterfront Campus, Southampton SO14 3ZH, Hants, England
[5] Univ Hawaii Manoa, Sch Ocean & Earth Sci & Technol, Hawaii Inst Geophys & Planetol, Honolulu, HI 96822 USA
[6] Ocean Floor Geophys, Burnaby, BC V5J 5J3, Canada
关键词
Gas and hydrate systems; Controlled source electromagnetics; Tomography; Inversion; Marine electromagnetics; Non-linear electromagnetics; WEST SVALBARD; POCKMARK; BENEATH; RIDGE; SEA; PRINCIPLES; SEDIMENTS; POROSITY; VELOCITY; SMOOTH;
D O I
10.1093/gji/ggy227
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
We present high-resolution resistivity imaging of gas hydrate pipe-like structures, as derived from marine controlled-source electromagnetic (CSEM) inversions that combine towed and ocean-bottom electric field receiver data, acquired from the Nyegga region, offshore Norway. 2.5-D CSEM inversions applied to the towed receiver data detected four new prominent vertical resistive features that are likely gas hydrate structures, located in proximity to a major gas hydrate pipe-like structure, known as the CNE03 pockmark. The resistivity model resulting from the CSEM data inversion resolved the CNE03 hydrate structure in high resolution, as inferred by comparison to seismically constrained inversions. Our results indicate that shallow gas hydrate vertical features can be delineated effectively by inverting both ocean-bottom and towed receiver CSEM data simultaneously. The approach applied here can be utilized to map and monitor seafloor mineralization, freshwater reservoirs, CO2 sequestration sites and near-surface geothermal systems.
引用
收藏
页码:1701 / 1714
页数:14
相关论文
共 99 条
[1]  
[Anonymous], 2009, 1 BREAK
[2]  
Archer D., 2007, Biogeosciences, V4, P521
[3]   Ocean methane hydrates as a slow tipping point in the global carbon cycle [J].
Archer, David ;
Buffett, Bruce ;
Brovkin, Victor .
PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA, 2009, 106 (49) :20596-20601
[4]  
Attias E., 2017, PANGAEA DATA PUBLISE, DOI 10.1594/PANGAEA.875644
[5]   Controlled-source electromagnetic and seismic delineation of subseafloor fluid flow structures in a gas hydrate province, offshore Norway [J].
Attias, Eric ;
Weitemeyer, Karen ;
Minshull, Tim A. ;
Best, Angus I. ;
Sinha, Martin ;
Jegen-Kulcsar, Marion ;
Hoelz, Sebastian ;
Berndt, Christian .
GEOPHYSICAL JOURNAL INTERNATIONAL, 2016, 206 (02) :1093-1110
[6]  
Boswell R., 2014, Methane Hydrates, Future Energy: Improved, Sustainable and Clean Options for Our Planet, Vsecond, P159
[7]  
Boswell R., 2015, INTERPRETATION, V4, pSA13
[8]   Current perspectives on gas hydrate resources [J].
Boswell, Ray ;
Collett, Timothy S. .
ENERGY & ENVIRONMENTAL SCIENCE, 2011, 4 (04) :1206-1215
[9]  
Chandola SK, 2014, INTERPRETATION-J SUB, V2, pSHI
[10]   A new marine controlled-source electromagnetic receiver with an acoustic telemetry modem and arm-folding mechanism [J].
Chen Kai ;
Wei Wenbo ;
Deng Ming ;
Wu Zhongliang ;
Yu Gang .
GEOPHYSICAL PROSPECTING, 2015, 63 (06) :1420-1429