Seismic fluid identification works as an effective approach to characterize the fluid feature
and distribution of the reservoir underground with seismic data. Rock physics which builds …

Seismic interpretation of mobile shales is challenging, mostly because of their unclear
seismic expression. Imaging of mobile shales is difficult because of their low seismic …

Recent research has established that the dominant P-wave attenuation mechanism in
reservoir rocks at seismic frequencies is because of wave-induced fluid flow (mesoscopic …

Remote seismic methods, which measure the compressional wave (P wave) velocity (Vp)
and shear wave (S wave) velocity (Vs), can be used to assess the distribution and …

The presence of gas hydrate in oceanic sediments is mostly identified by bottom-simulating
reflectors (BSRs), reflection events with reversed polarity following the trend of the seafloor …

We present a new petro-elastical and numerical-simulation methodology to compute
synthetic seismograms for reservoirs subject to CO 2 sequestration. The petro-elastical …

Shale source rocks are composed of various minerals, mainly smectite and illite, depending
on the burial depth, and they can be described as transversely isotropic media. The “pore …

Source rocks are described by a porous transversely isotropic medium composed of illite
and organic matter (kerogen, oil, and gas). The bulk modulus of the oil/gas mixture is …

Indian National Gas Hydrate Program Expedition 01 has established that clay‐rich marine
sediment from the Krishna‐Godavari (KG) basin in the eastern Indian margin hosts one of …

Analysis of P wave velocities of an ocean‐bottom cable (OBC) data set demonstrates the
existence of gas hydrates and free gas on the northern flank of the Storegga Slide. The …