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Supplemental material: Provenance of the Paleogene Colton Formation (Uinta Basin) and Cretaceous–Paleogene provenance evolution in the Utah foreland: Evidence from U-Pb ages of detrital zircons, paleocurrent trends, and sandstone petrofacies

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posted on 2012-06-26, 00:00 authored by William R. Dickinson, Timothy F. Lawton, Mark Pecha, Steven J. Davis, George E. Gehrels, Richard A. Young
Geosphere, August 2012, v. 8, p. 854-880, doi:10.1130/GES00763.1, Supplemental File 1 - Word file of Detrital Zircon (DZ) Sample Localities.

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Provenance of the Paleogene Colton Formation (Uinta Basin) and Cretaceous–Paleogene provenance evolution in the Utah foreland: Evidence from U-Pb ages of detrital zircons, paleocurrent trends, and sandstone petrofacies
GeosphereGeosphere

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