Abstract: The discontinuity surface between Earth crust and mantle, the so-called Moho, is commonly estimated by means of seismic or gravimetric methods. Usually these methods do not yield the same ...

Lateral variations of crustal thickness and Vp/Vs ratio are inferred from both H-k and common conversion point stacks. We observe long-wavelength variations of Moho depth from ∼31 km in the Thrace ...

Mexico City is no stranger to seismic events, feeling the effects of both shallow crustal earthquakes and deeper subduction earthquakes. "The large ground accelerations shown by the recent small ...

Scripps Institution of Oceanography, University of California San Diego, La Jolla, CA, United States ...