Integration of regional stratigraphic relationships with data on sediment accumulation,
provenance, paleodrainage, and deformation timing enables a reconstruction of Mesozoic …

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 …

Geochronological, structural, and sedimentological data provide the basis for a regional
synthesis of the evolution of the Cordilleran retroarc thrust belt and foreland basin system in …

The processes of erosion and deposition must be included in foreland basin models to
predict correctly basin geometry and stratigraphy. We present a synthetic stratigraphic model …

The crust of the Great Basin has occupied a range of tectonic settings through geologic time.
Archean and Paleoproterozoic crustal genesis preceded residence of Laurentia within the …

Abstract The Canyon Range, Pavant, Paxton, and Gunnison thrust systems in central Utah
form the Sevier fold-and-thrust belt in its type area. The Canyon Range thrust carries an∼ …

Tectonic setting exerts first-order control on basin formation as reflected in basin subsidence
history. While our approach ignores the effects of flexural loading and eustatic sea-level …

We incorporate the processes of erosion and deposition in a numerical model to predict the
stratal geometries and facies patterns produced during episodic thrusting in a nonmarine …

In late Mesozoic time, the southern Cordilleran foreland basin was bounded on the west by
the Sevier thrust belt and on the south by the Mogollon highlands. Paleocurrent indicators in …

Actualistic plate‐tectonic models are the best framework within which to understand the
tectonics of sedimentary basins. Sedimentary basins develop in divergent, intraplate …