Abstract Crustal structure in South America is one of the least understood among the Earth's
continental areas. Variations in crustal thickness are still poorly constrained over large …

A non-linear Bayesian Monte-Carlo method is presented to estimate a Vsv model beneath
stations by jointly interpreting Rayleigh wave dispersion and receiver functions and …

We compare 12 recent three-dimensional (3D) seismic imaging results that made extensive
use of data from the Earthscope Transportable Array (TA). Our goal is to sort out what can be …

In 2010, the Incorporated Research Institutions for Seismology (IRIS) Data Management
Center (DMC) expanded the preexisting effort to generate, archive, and distribute data …

Large-scale deformation of continents remains poorly understood more than 40 years after
the plate tectonic revolution. Rock flow strength and mass density variations both contribute …

To better constrain the temperature structure in the upper mantle, we jointly invert seismic
surface wave velocities and basalt thermobarometry. New measurements of the water …

We have developed a new method to retrieve seismic surface wave phase velocity using
dense seismic arrays. The method measures phase variations between nearby stations …

A new tomographic S wave velocity model for the upper mantle beneath South America is
presented. We developed and applied a new method of simultaneously inverting regional S …

Low‐velocity sedimentary basins introduce error in many standard receiver‐function (RF)
analysis techniques including common conversion point (Dueker and Sheehan, 1997) and …

In an earlier study, Bensen et al. measured surface wave dispersion curves from ambient
noise using 203 stations across North America, which resulted in Rayleigh and Love wave …