Broken foreland basins are caused by crustal-scale contractional basement structures that
compartmentalize (or break) a contiguous retroarc or collisional foreland basin into smaller …

Defining the structural style of fold–thrust belts and understanding the controlling factors are
necessary steps towards prediction of their long-term and short-term dynamics, including …

Quantifying the kinematic evolution of an orogenic system, recorded in its 3-D displacement
field, across a range of spatial and temporal scales is challenging, yet crucial for quantifying …

This paper combines the power of deep‐learning with the generalizability of physics‐based
features, to present an advanced method for seismic discrimination between earthquakes …

A new 3-D resistivity model, estimated from inversion of magnetotelluric data, images crustal
and upper-mantle structure of the Wyoming Province and adjacent areas. The Archean …

The Laramide foreland belt comprises a broad region of thick-skinned, contractional
deformation characterized by an anastomosing network of basement-cored arches and …

Although accurately classifying signals from earthquakes and explosions at local distance (<
250 km) remains an important task for seismic network operations, the growing volume of …

Continental fold‐thrust belts display a variety of structural styles, ranging from thin‐skinned
thrusts following weak lithologic contacts to thick‐skinned thrusts that deform mechanical …

Moho topography yields insights into the evolution of the lithosphere and the strength of the
lower crust. The Moho reflected phase (PmP) samples this key boundary and may be used …

The idea of using a deep autoencoder to encode seismic waveform features and then use
them in different seismological applications is appealing. In this paper, we designed tests to …