U-Pb detrital zircon analyses provide a new maximum depositional age constraint on the Uinta Mountain Group (UMG) and correlative Big Cottonwood Formation (BCF) of Utah, and significantly enhance our insights on the mid-Neoproterozoic paleogeographic an
Detailed analysis of the basal unit of the Uinta Mountain Group, the Jesse Ewing Canyon Formation, o...
During the earliest 40% of Tertiary time, from about 65 to 40 million years ago, much of the Uinta B...
The landscape evolution of the northeastern Uinta Mountains and the manner in which climatic and tec...
U–Pb ages of detrital zircon spectra indicate that the Little Willow Formation in the Wasatch Range,...
The upper Tonian ChUMP (Chuar-Uinta Mountains-Pahrump) strata of the southwestern U.S.A. are hypothe...
Geologic mapping, facies analysis, sedimentary petrography, and detrital zircon analyses of undivide...
In order to better constrain the age and provenance of the Upper Cretaceous Wahweap and Kaiparowits ...
Stratigraphic, geochronologic, and geochemical patterns of Neoproterozoic to Cambrian sedimentary an...
The Bear River Range in Northern Utah is composed of a thick succession of Paleozoic strata. Limesto...
Constraining the depositional age of Neoproterozoic stratigraphy in western North America has implic...
Three stratigraphically well defined rocks from the glaciogenic Scout Mountain Member, Neoproterozoi...
Detangling the pace and structure of biotic turnover between the late Early and early Late Cretaceou...
This research is focused on rock units deposited in northern Utah before and after global glacial ev...
Three related sedimentary successions located in Arizona, Utah, and California were deposited in bas...
Volcanic and diamictite-bearing strata of the Neoproterozoic Pocatello Formation record middle Cryog...
Detailed analysis of the basal unit of the Uinta Mountain Group, the Jesse Ewing Canyon Formation, o...
During the earliest 40% of Tertiary time, from about 65 to 40 million years ago, much of the Uinta B...
The landscape evolution of the northeastern Uinta Mountains and the manner in which climatic and tec...
U–Pb ages of detrital zircon spectra indicate that the Little Willow Formation in the Wasatch Range,...
The upper Tonian ChUMP (Chuar-Uinta Mountains-Pahrump) strata of the southwestern U.S.A. are hypothe...
Geologic mapping, facies analysis, sedimentary petrography, and detrital zircon analyses of undivide...
In order to better constrain the age and provenance of the Upper Cretaceous Wahweap and Kaiparowits ...
Stratigraphic, geochronologic, and geochemical patterns of Neoproterozoic to Cambrian sedimentary an...
The Bear River Range in Northern Utah is composed of a thick succession of Paleozoic strata. Limesto...
Constraining the depositional age of Neoproterozoic stratigraphy in western North America has implic...
Three stratigraphically well defined rocks from the glaciogenic Scout Mountain Member, Neoproterozoi...
Detangling the pace and structure of biotic turnover between the late Early and early Late Cretaceou...
This research is focused on rock units deposited in northern Utah before and after global glacial ev...
Three related sedimentary successions located in Arizona, Utah, and California were deposited in bas...
Volcanic and diamictite-bearing strata of the Neoproterozoic Pocatello Formation record middle Cryog...
Detailed analysis of the basal unit of the Uinta Mountain Group, the Jesse Ewing Canyon Formation, o...
During the earliest 40% of Tertiary time, from about 65 to 40 million years ago, much of the Uinta B...
The landscape evolution of the northeastern Uinta Mountains and the manner in which climatic and tec...