The thin-skin Sevier and thick-skin Laramide belts of the North American Cordillera provide
a long-term record of the interrelations between evolving styles of mountain building and …

This paper gives an overview of the large-scale tectonic styles encountered in orogens
worldwide. Thin-skinned and thick-skinned tectonics represent two end member styles …

This paper presents a new model of the shear velocity structure of the crust and uppermost
mantle beneath the contiguous US The model is based on more than a decade of USArray …

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 …

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 …

With its central position between the Tibetan Plateau and the Tian Shan Range, the Tarim
Basin is a key element of the Cenozoic Asian orogenic system. However, a comprehensive …

Seismic structure beneath the contiguous US was imaged with multimode receiver function
stacking and inversion of Rayleigh wave dispersion and ellipticity measurements. Crust …

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 …

Converted wave imaging has revealed significant negative velocity gradients, often termed
midlithospheric discontinuities, within the thick, high‐velocity mantle beneath cratons. In this …

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