 | mantle convection; plate tectonics; structural seismology; numerical modeling; earthquakes; fluid dynamics
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 | Please see https://catloslab.org/
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 | Tectonics of sedimentary basins, evolution of orogenic systems, sediment provenance and routing systems, nonmarine depositional processes.
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 | Field-based Structural Geology; Paleomagnetism; Plate Reconstruction; U-Pb Zircon Geochronology; Orogenic Systems; Planetary Geology
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 | Thermo-/Geochronology, Tectonics and Structural Geology, Isotopic Provenance Analysis, Archeometry, Geothermal Exploration, and Thermal Maturation
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 | OCEEMlab focuses on mitigating climate-driven phenomena by studying dynamic processes at oceanic plate boundaries, addressing geohazards, and promoting a New Blue Economy.
Research Interests: (1) The interplay between mantle plumes, submarine freshwater, and marine biodiversity in volcanic systems. (2) Hot-spot mantle plume geodynamics and submarine volcanism. (3) Slab rollback-driven toroidal and poloidal mantle ...
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 | Stratigraphic evolution of a wide range of marine and lacustrine environments around the world
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 | Salt tectonics, 3-D computer modeling, kinematic models for evolution and growth of salt structures, structural geology, cross-section restoration and balancing, seismic interpretation
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| Crustal deformation, GPS/Geodesy, active plate boundary processes, subduction tectonics, geohazards
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 | Marine geophysics, plate tectonics, magnetics, gravity, heat flow, seismic studies, paleogeographic reconstructions of Gondwana, the Polar Regions, East Asia, and the Western Pacific
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 | Vertebrate paleontology, evolution and development of the vertebrate skeleton, phylogenetic systematics, the early history of mammals and their extinct relatives among Synapsida, the history of birds and their extinct relatives among Dinosauria, the history of other amniotes, high-resolution X-ray computed tomography, CT scanner, DigiMorph, informatics
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 | Tectonic geomorphology, stratigraphy, and paleogeodesy/paleoseismology at convergent plate margins
Paleoclimate, fossil corals as a proxy for past sea-surface temperatures. Corals as recorders of relative sea level for vertical tectonics and sea-level history.
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