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 …

Abstract The North American Cordilleran Anatectic Belt (CAB) is a~ 3,000 km long region in
the hinterland of the Cordillera that comprises numerous exposures of Late Cretaceous to …

Surface velocities derived from GPS observations from 1993 to 2011 at several hundred
sites across the deforming northwestern United States are used to further elucidate the …

New high-resolution P-and S-wave tomography of the United States upper mantle from the
Pacific Coast to the Great Plains reveals strong multi-scale heterogeneity closely correlated …

A major plate reorganization is postulated to have occurred at approximately 100Ma.
However, this reorganization has received limited attention, despite being associated with …

The Idaho batholith and spatially overlapping Challis intrusive province in the North
American Cordillera have a history of magmatism spanning some 55 Myr. New isotopic data …

We present a compilation of 8717 U‐Pb analyses from 95 detrital zircon samples of Jurassic‐
Eocene North American Cordillera foreland basin strata. Of these samples, 30 are new and …

Teleseismic tomography images a large high-velocity “curtain” extending vertically beneath
the ca. 50 Ma Challis magmatic trend to maximum depths of 230–600 km. We interpret this …

Timing and distribution of magmatism, deformation, exhumation, and basin development
have been used to reconstruct the history of Laramide flat‐slab subduction under North …

Integrated geochemical, isotopic, and geochronological constraints from Jurassic plutonic
rocks of the Central Cordillera in Colombia were used to determine the tectonic setting and …