Area of research
Geophysics · Artificial Intelligence
Research interest
Research interests include Geology, Zircon, Geochronology, Provenance, Cenozoic, and Paleontology.
An exploratory study of “large‐ <i>n</i> ” detrital zircon geochronology of the Book Cliffs, <scp>UT</scp> via rapid (3 s/analysis) <scp>U–Pb</scp> dating
Basin formation, magmatism, and exhumation document southward migrating flat-slab subduction in the central Andes
Episodic Late Cretaceous to Neogene crustal thickness variation in southern Tibet
Large detrital zircon data set investigation and provenance mapping: Local versus regional and continental sediment sources before, during, and after Ancestral Rocky Mountain deformation
Crustal Thickening of the Northern Central Andean Plateau Inferred From Trace Elements in Zircon
Linking the Gulf of Mexico and Coast Mountains batholith during late Paleocene time: Insights from Hf isotopes in detrital zircons
Jurassic to Neogene Quantitative Crustal Thickness Estimates in Southern Tibet
Two‐Dimensional Quantitative Comparison of Density Distributions in Detrital Geochronology and Geochemistry
Detrital sanidine 40Ar/39Ar dating confirms &lt;2 Ma age of Crooked Ridge paleoriver and subsequent deep denudation of the southwestern Colorado Plateau
Rapid U‐Pb Geochronology by Laser Ablation Multi‐Collector ICP‐MS
Detrital zircons and sediment dispersal in the eastern Midcontinent of North America
Laramide Orogenesis Driven by Late Cretaceous Weakening of the North American Lithosphere
Detrital-zircon analyses, provenance, and late Paleozoic sediment dispersal in the context of tectonic evolution of the Ouachita orogen
Implications of variable late Cenozoic surface uplift across the Peruvian central Andes
Provenance and recycling of detrital zircons from Cenozoic Altiplano strata and the crustal evolution of western South America from combined U-Pb and Lu-Hf isotopic analysis
Characterizing sediment sources by non-negative matrix factorization of detrital geochronological data
Detrital zircons and sediment dispersal from the Coahuila terrane of northern Mexico into the Marathon foreland of the southern Midcontinent
Peruvian Altiplano Stratigraphy Highlights Along‐Strike Variability in Foreland Basin Evolution of the Cenozoic Central Andes
Evidence for constriction and Pliocene acceleration of east‐west extension in the North Lunggar rift region of west central Tibet