By harnessing both hypothetical, synthetic basin and gas hydrate (GH) system models and
real‐world models of well‐studied salt diapir‐associated GH sites at Green Canyon (Gulf of …

Modern observations and geological records suggest that anthropogenic ocean warming
could destabilise marine methane hydrate, resulting in methane release from the seafloor to …

Gas hydrates are one of the largest marine carbon reservoirs on Earth. The conventional
understanding of hydrate dynamics assumes that the system, in the absence of external …

We explored methane hydrate formation with sedimentation with a newly developed one‐
dimensional, multiphase flow, multicomponent transport numerical model. Our model …

The basin-scale distribution of gas hydrates and methane migration pathways in the western
Black Sea remains enigmatic, owing to the region's complex geological history …

A new numerical model reconstructing the depositional history (98–0 Ma) of the Western
Black Sea sub-basin is presented. The model accounts for changing boundary conditions (ie …

The natural gas hydrates detected in Shenhu Area, South China Sea are considered to have
great potential for exploitation and to become a research hotspot. However, details of the …

A site at the gas hydrate stability limit was investigated offshore northwestern Svalbard to
study methane transport in sediment. The site was characterized by chemosynthetic …

Methane hydrates are solid structures containing methane inside of a water lattice that form
under low temperature and relatively high pressure. Appropriate hydrate‐forming conditions …

Rapid sedimentation reduces the temperature and raises the pore pressure in sedimentary
basins. During rapid sedimentation (> 0.5 mm yr− 1), cold sediment is buried fast and there …