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  4. Three-dimensional distribution of gas hydrate beneath southern Hydrate Ridge: Constraints from ODP Leg 204
 
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Three-dimensional distribution of gas hydrate beneath southern Hydrate Ridge: Constraints from ODP Leg 204

Journal
Earth and Planetary Science Letters
Journal Volume
222
Journal Issue
3-4
Pages
845-862
Date Issued
2004
Author(s)
CHAR-SHINE LIU  
DOI
10.1016/j.epsl.2004.03.035
URI
http://www.scopus.com/inward/record.url?eid=2-s2.0-18144451669&partnerID=MN8TOARS
http://scholars.lib.ntu.edu.tw/handle/123456789/308860
Abstract
Large uncertainties about the energy resource potential and role in global climate change of gas hydrates result from uncertainty about how much hydrate is contained in marine sediments. During Leg 204 of the Ocean Drilling Program (ODP) to the accretionary complex of the Cascadia subduction zone, we sampled the gas hydrate stability zone (GHSZ) from the seafloor to its base in contrasting geological settings defined by a 3D seismic survey. By integrating results from different methods, including several new techniques developed for Leg 204, we overcome the problem of spatial under-sampling inherent in robust methods traditionally used for estimating the hydrate content of cores and obtain a high-resolution, quantitative estimate of the total amount and spatial variability of gas hydrate in this structural system. We conclude that high gas hydrate content (30-40% of pore space or 20-26% of total volume) is restricted to the upper tens of meters below the seafloor near the summit of the structure, where vigorous fluid venting occurs. Elsewhere, the average gas hydrate content of the sediments in the gas hydrate stability zone is generally <2% of the pore space, although this estimate may increase by a factor of 2 when patchy zones of locally higher gas hydrate content are included in the calculation. These patchy zones are structurally and stratigraphically controlled, contain up to 20% hydrate in the pore space when averaged over zones ∼10 m thick, and may occur in up to ∼20% of the region imaged by 3D seismic data. This heterogeneous gas hydrate distribution is an important constraint on models of gas hydrate formation in marine sediments and the response of the sediments to tectonic and environmental change. © 2004 Published by Elsevier B.V.
Subjects
Accretionary margins; Gas hydrates; Marine sediments; Methane; Ocean Drilling Program
SDGs

[SDGs]SDG13

[SDGs]SDG14

Other Subjects
gas hydrate; methane; Ocean Drilling Program; resource assessment; spatial distribution; three-dimensional modeling; Cascadia Margin; Hydrate Ridge; Pacific Ocean
Type
journal article

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