Marine-controlled source electromagnetic study of methane seeps and gas hydrates at Opouawe Bank, Hikurangi Margin, New Zealand.

Schwalenberg, Katrin, Rippe, Dennis, Koch, Stephanie and Scholl, Carsten (2017) Marine-controlled source electromagnetic study of methane seeps and gas hydrates at Opouawe Bank, Hikurangi Margin, New Zealand. Open Access Journal of Geophysical Research: Solid Earth, 122 (5). pp. 3334-3350. DOI 10.1002/2016JB013702.

[img]
Preview
Text
jgrb52067.pdf - Published Version

Download (8Mb) | Preview

Supplementary data:

Abstract

Marine controlled source electromagnetic (CSEM) data have been collected to investigate methane seep sites and associated gas hydrate deposits at Opouawe Bank on the southern tip of the Hikurangi Margin, New Zealand. The bank is located in about 1000 m water depth within the gas hydrate stability field. The seep sites are characterized by active venting and typical methane seep fauna accompanied with patchy carbonate outcrops at the seafloor. Below the seeps, gas migration pathways reach from below the bottom-simulating reflector (at around 380 m sediment depth) toward the seafloor, indicating free gas transport into the shallow hydrate stability field. The CSEM data have been acquired with a seafloor-towed, electric multi-dipole system measuring the inline component of the electric field. CSEM data from three profiles have been analyzed by using 1-D and 2-D inversion techniques. High-resolution 2-D and 3-D multichannel seismic data have been collected in the same area. The electrical resistivity models show several zones of highly anomalous resistivities (>50 Ωm) which correlate with high amplitude reflections located on top of narrow vertical gas conduits, indicating the coexistence of free gas and gas hydrates within the hydrate stability zone. Away from the seeps the CSEM models show normal background resistivities between ~1 and 2 Ωm. Archie's law has been applied to estimate gas/gas hydrate saturations below the seeps. At intermediate depths between 50 and 200 m below seafloor, saturations are between 40 and 80% and gas hydrate may be the dominating pore filling constituent. At shallow depths from 10 m to the seafloor, free gas dominates as seismic data and gas plumes suggest.

Document Type: Article
Additional Information: Metadata of cruise SO214 are available from SeaDataNet.org.
Keywords: marine CSEM; gas hydrates; methane seepage; Opouawe Bank; NZ
Research affiliation: GFZ
OceanRep > GEOMAR > FB4 Dynamics of the Ocean Floor > FB4-GDY Marine Geodynamics
Refereed: Yes
Open Access Journal?: No
DOI etc.: 10.1002/2016JB013702
ISSN: 0148-0227
Expeditions/Models/Experiments:
Date Deposited: 19 Jun 2017 08:26
Last Modified: 01 Feb 2019 15:09
URI: http://oceanrep.geomar.de/id/eprint/38425

Actions (login required)

View Item View Item

Document Downloads

More statistics for this item...