Open AccessGeological Controls on Fluid Flow and Gas Hydrate Pingo Development on the Barents Sea Margin
Author(s) -
Waage M.,
Portnov A.,
Serov P.,
Bünz S.,
Waghorn K. A.,
Vadakkepuliyambatta S.,
Mienert J.,
Andreassen K.
Publication year - 2019
Publication title -
geochemistry, geophysics, geosystems
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.928
H-Index - 136
ISSN - 1525-2027
DOI - 10.1029/2018gc007930
Subject(s) - geology , clathrate hydrate , seafloor spreading , mud volcano , sedimentary rock , methane , geochemistry , seabed , glacial period , petroleum seep , continental shelf , cold seep , fault (geology) , petrology , geomorphology , hydrate , oceanography , seismology , ecology , chemistry , organic chemistry , biology
Abstract In 2014, the discovery of seafloor mounds leaking methane gas into the water column in the northwestern Barents Sea became the first to document the existence of nonpermafrost‐related gas hydrate pingos (GHPs) on the Eurasian Arctic shelf. The discovered site is given attention because the gas hydrates occur close to the upper limit of the gas hydrate stability, thus may be vulnerable to climatic forcing. In addition, this site lies on the regional Hornsund Fault Zone marking a transition between the oceanic and continental crust. The Hornsund Fault Zone is known to coincide with an extensive seafloor gas seepage area; however, until now lack of seismic data prevented connecting deep structural elements to shallow seepages. Here we use high‐resolution P‐Cable 3‐D seismic data to study the subsurface architecture of GHPs and underlying glacial and preglacial deposits. The data show gas hydrates, authigenic carbonates, and free gas within the GHPs on top of gas chimneys piercing a thin section of low‐permeability glacial sediments. The chimneys connect to faults within the underlying tilted and folded fluid and gas‐hydrate‐bearing sedimentary rocks. Correlation of our data with regional 2‐D seismic surveys shows a spatial connection between the shallow subsurface fluid flow system and the deep‐seated regional fault zone. We suggest that fault‐controlled Paleocene hydrocarbon reservoirs inject methane into the low‐permeability glacial deposits and near‐seabed sediments, forming the GHPs. This conceptual model explains the existence of climate‐sensitive gas hydrate inventories and extensive seabed methane release observed along the Svalbard‐Barents Sea margin.