Gas hydrates (GH) are well known to have an influential effect on the velocity and
attenuation of gas hydrate-bearing sediments (GHBS). Based on rock physics modeling …

Understanding the magmatic plumbing system of rift volcanoes is essential when examining
the interplay between magmatic and tectonic forces. Recent seismicity, volcanic activity …

Using the forced oscillation method, we measure the extensional‐mode attenuation and
Young's modulus of a Berea sandstone sample at seismic frequencies (0.5–50 Hz) for …

The frequency dependence of seismic properties of fully saturated rocks can be related to
wave‐induced fluid flows at different scales. The elastic dispersion and attenuation of four …

Quantitatively assessing seismic attenuation caused by fluid pressure diffusion (FPD) in
partially saturated rocks is challenging because of its sensitivity to the spatial fluid …

Despite their importance for eruption forecasting the causes of seismic rupture processes
during caldera unrest are still poorly reconstructed from seismic images. Seismic source …

The majority of presently exploitable marine methane hydrate reservoirs are likely to host
hydrate in disseminated form in coarse grain sediments. For hydrate concentrations below …

Mapping fluid accumulation in the crust is pertinent for numerous applications including
volcanic hazard assessment, geothermal energy generation, and mineral exploration. Here …

Because measuring the frequency dependence of elastic properties in the laboratory is a
technical challenge, not enough experimental data exist to test the existing theories. We …

Understanding the effects of pressure and rock microstructure on seismic elastic properties
of fully saturated rocks is of considerable importance in a range of geophysical applications …