The Barents Sea, located close to the Arctic Ocean, is a petroleum province featuring an extensive occurrence of gas hydrates and shallow gas in compacted sediments. Glacial erosion and uplift have contributed to the migration of gas originating from deeper rocks to the shallow sediments of this region, resulting in hydrates with higher-order hydrocarbons in addition to methane. This article documents reported gas hydrate indications and major controls on hydrate stability in the Barents Sea
Recent estimations suggest that vast amounts of methane are locked in the Arctic Ocean bottom sedime...
Recent estimations suggest that vast amounts of methane are locked in the Arctic Ocean bottom sedime...
The Barents Sea is a large epicontinental sea and petroliferous basin, which is fairly unexplored co...
The Barents Sea is a major part of the Arctic where the Gulf Stream mixes with the cold Arctic water...
The SW Barents Sea is a large hydrocarbon-prone epicontinental Sea comprised of a complex mosaic of ...
In 2014, the discovery of seafloor mounds leaking methane gas into the water column in the northwest...
The ongoing warming of bottom water in the Arctic region is anticipated to destabilize some of the g...
A widespread bottom-simulating reflection (BSR) defining the base of the gas hydrate stability zone ...
Gas hydrates store a large amount of methane (>500 Gt of Carbon) in continental margins and permafro...
In this study we assess the present-day gas hydrate stability zone for the Barents Sea and Kara Sea ...
AbstractIn this study we assess the present-day gas hydrate stability zone for the Barents Sea and K...
Gas hydrates (GH) are perspective energy sources, containing significantly more gas resources compar...
Submarine gas hydrates are ice-like solid structures form from pore water and natural gases [Brooks,...
Deep sea methane hydrates are found several hundred metres beneath the continental slopes of many ar...
Recent estimations suggest that vast amounts of methane are locked in the Arctic Ocean bottom sedime...
Recent estimations suggest that vast amounts of methane are locked in the Arctic Ocean bottom sedime...
Recent estimations suggest that vast amounts of methane are locked in the Arctic Ocean bottom sedime...
The Barents Sea is a large epicontinental sea and petroliferous basin, which is fairly unexplored co...
The Barents Sea is a major part of the Arctic where the Gulf Stream mixes with the cold Arctic water...
The SW Barents Sea is a large hydrocarbon-prone epicontinental Sea comprised of a complex mosaic of ...
In 2014, the discovery of seafloor mounds leaking methane gas into the water column in the northwest...
The ongoing warming of bottom water in the Arctic region is anticipated to destabilize some of the g...
A widespread bottom-simulating reflection (BSR) defining the base of the gas hydrate stability zone ...
Gas hydrates store a large amount of methane (>500 Gt of Carbon) in continental margins and permafro...
In this study we assess the present-day gas hydrate stability zone for the Barents Sea and Kara Sea ...
AbstractIn this study we assess the present-day gas hydrate stability zone for the Barents Sea and K...
Gas hydrates (GH) are perspective energy sources, containing significantly more gas resources compar...
Submarine gas hydrates are ice-like solid structures form from pore water and natural gases [Brooks,...
Deep sea methane hydrates are found several hundred metres beneath the continental slopes of many ar...
Recent estimations suggest that vast amounts of methane are locked in the Arctic Ocean bottom sedime...
Recent estimations suggest that vast amounts of methane are locked in the Arctic Ocean bottom sedime...
Recent estimations suggest that vast amounts of methane are locked in the Arctic Ocean bottom sedime...
The Barents Sea is a large epicontinental sea and petroliferous basin, which is fairly unexplored co...