Area of research
Geophysics · Artificial Intelligence
Research interest
Research interests include Geology, Paleontology, Foreland basin, Subduction, Provenance, and Plateau (mathematics).
Broken foreland basins and the influence of subduction dynamics, tectonic inheritance, and mechanical triggers
Aseismic ridge subduction focused late Cenozoic exhumation above the Peruvian flat slab
Causes of Variable Shortening and Tectonic Subsidence During Changes in Subduction: Insights From Flexural Thermokinematic Modeling of the Neogene Southern Central Andes (28–30°S)
Did accretion of the Caribbean oceanic plateau drive rapidcrustal thickening in the northern Andes?
Andean Mountain Building and Foreland Basin Evolution During Thin‐ and Thick‐Skinned Neogene Deformation (32–33°S)
Thermochronological and Geochronological Constraints on Late Cretaceous Unroofing and Proximal Sedimentation in the Sevier Orogenic Belt, Utah
Implications of variable late Cenozoic surface uplift across the Peruvian central Andes
Orogenic Wedge Evolution of the Central Andes, Bolivia (21°S): Implications for Cordilleran Cyclicity
Mesozoic to Cenozoic retroarc basin evolution during changes in tectonic regime, southern Central Andes (31–33°S): Insights from zircon U-Pb geochronology
Tectonic Evolution of the Central Andean Plateau and Implications for the Growth of Plateaus
Neogene shortening and exhumation of the Zagros fold-thrust belt and foreland basin in the Kurdistan region of northern Iraq
The Miocene Arizaro Basin, central Andean hinterland: Response to partial lithosphere removal?
Inversion tectonics under increasing rates of shortening and sedimentation: Cenozoic example from the Eastern Cordillera of Colombia
On the lag time between internal strain and basement involved thrust induced exhumation: The case of the Colombian Eastern Cordillera
Provenance of the Paleocene-Eocene Wilcox Group, western Gulf of Mexico basin: Evidence for integrated drainage of the southern Laramide Rocky Mountains and Cordilleran arc
Late Cenozoic evolution of the Lunggar extensional basin, Tibet: Implications for basin growth and exhumation in hinterland plateaus