The time-frequency (TF) analysis method plays a significant role in the detection of natural
gas hydrates. As a data-driven method, compressed sensing (CS) has been widely used in …

Gas transport through sediments to the seabed and seepage occurs via advection through
pores, faults, and fractures, and as solubility driven gas diffusion. The pore pressure gradient …

Abstract In the Fram Strait, mid‐ocean ridge spreading is represented by the ultra‐slow
system of the Molloy Ridge, the Molloy Transform Fault and the Knipovich Ridge. Sediments …

Gas hydrates occur within sediments on the western Svalbard continental margin and the
Vestnesa Ridge, a large sediment drift that extends in a west‐northwest direction from the …

Joint analysis of electrical resistivity and seismic velocity data is primarily used to detect the
presence of gas hydrate‐filled faults and fractures. In this study, we present a novel …

Recent studies have confirmed the coexistence of gas hydrate (GH) and free gas (FG) in gas
hydrate stability zone (GHSZ). However, the acoustic properties of the coexisting sediment …

Quality factor (Q) or equivalently attenuation describes the amount of energy lost per cycle
as a wave travels through a medium. This is important to correct seismic data amplitudes for …

Frenulate species were identified from a high Arctic methane seep area on Vestnesa Ridge,
western Svalbard margin (79° N, Fram Strait) based on mitochondrial cytochrome oxidase …

Cap rock is any impermeable or low permeability formation that may trap oil, gas or water,
preventing it from migrating to the surface. Evaluation of sealing properties of the cap rock is …

Wave velocity and attenuation of gas hydrate-bearing samples are often extrapolated from
ultrasonic to lower seismic/sonic frequencies, but the impact of measurement frequency on …