Phase D, an elastically anisotropic hydrous mineral, is stable around cold subducting slabs at depths of mid mantle, potentially being the source of seismic anisotropy.

The Oklahoma Geological Survey is wanting to double the size of their data network. In order to do that, they need landowners ...

Seismic waves from earthquakes have always offered a window into Earth’s hidden interior. For decades, researchers believed ...

Ground motion is registered in several seismic stations across Finland. Data are automatically processed at Institute of Seismology: signals caused by explosions, earthquakes and collapses are ...