Anomalous porosity preservation and preferential accumulation of gas hydrate in the Andaman accretionary wedge, NGHP-01 site 17A

In addition to well established properties that control the presence or absence of the hydrate stability zone, such as pressure, temperature, and salinity, additional parameters appear to influence the concentration of gas hydrate in host sediments. The stratigraphic record at Site 17A in the Andama...

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Bibliographic Details
Published in:Marine and petroleum geology 2014-12, Vol.58, p.99-116
Main Authors: Rose, Kelly K., Johnson, Joel E., Torres, Marta E., Hong, Wei-Li, Giosan, Liviu, Solomon, Evan A., Kastner, Miriam, Cawthern, Thomas, Long, Philip E., Todd Schaef, H.
Format: Article
Language:English
Subjects:
Carbonate
Gas hydrate
Gas hydrates
Grain size
Indian Ocean
Marine
Minerals
Permeability
Porosity
Preservation
Saturation
Sediments
Volcanic ash
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Summary:In addition to well established properties that control the presence or absence of the hydrate stability zone, such as pressure, temperature, and salinity, additional parameters appear to influence the concentration of gas hydrate in host sediments. The stratigraphic record at Site 17A in the Andaman Sea, eastern Indian Ocean, illustrates the need to better understand the role pore-scale phenomena play in the distribution and presence of marine gas hydrates in a variety of subsurface settings. In this paper we integrate field-generated datasets with newly acquired sedimentology, physical property, imaging and geochemical data with mineral saturation and ion activity products of key mineral phases such as amorphous silica and calcite, to document the presence and nature of secondary precipitates that contributed to anomalous porosity preservation at Site 17A in the Andaman Sea. This study demonstrates the importance of grain-scale subsurface heterogeneities in controlling the occurrence and distribution of concentrated gas hydrate accumulations in marine sediments, and document the importance that increased permeability and enhanced porosity play in supporting gas concentrations sufficient to support gas hydrate formation. The grain scale relationships between porosity, permeability, and gas hydrate saturation documented at Site 17A likely offer insights into what may control the occurrence and distribution of gas hydrate in other sedimentary settings. •Documented relationship primary and secondary sedimentary framework at Site 17A.•Secondary sedimentary framework influenced distribution of gas hydrates at Site 17A.•Secondary micro-crystalline carbonates led to enhanced porosity preservation.•Secondary porosity likely also enhanced permeability, influencing gas migration.•Coarser grained lithofacies associated with enhanced porosity have more gas hydrate.
ISSN:0264-8172
1873-4073
DOI:10.1016/j.marpetgeo.2014.04.009