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

As zircon U-Pb geochronology has become a leading method in sediment provenance
studies and basin analysis over the past 20 years, the volume of detrital zircon data made …

This paper explores an inverse approach to the problem of characterizing sediment
sources'(“source” samples) age distributions based on samples from a particular depocenter …

Detrital zircon U-Pb studies of mudstone provenance are rare but may preferentially
fingerprint distal zircon sources. To examine this issue, Pierre Shale and Trinidad …

Abstract Late Cretaceous to Eocene Laramide basement–involved shortening fragmented
the Sevier and Mexican foreland basins. This resulted in a major drainage reorganization in …

Detrital zircon surface microtextures, geochronologic U‐Pb data, and tectonic subsidence
analysis from Upper Jurassic to Paleocene strata in the Black Hills of South Dakota reveal …

The stratigraphic record from the North American Cordilleran foreland basin (CFB) serves as
a critical archive of how tectonics, sea level, and sediment supply interacted throughout the …

Cretaceous through Eocene strata of the Four Corners region provide an excellent record of
changes in sediment provenance from Sevier thin-skinned thrusting through the formation of …

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

Dynamic topography refers to the vertical deflection (ie, uplift and subsidence) of the Earth's
surface generated in response to mantle flow. Although dynamic subsidence has been …