CL
Member Since 1988
Carolina R. Lithgow-Bertelloni
Full Professor, University of California Los Angeles
AGU Research
Search
Filters
Clear All
How Phase Transitions Impact Changes in Mantle Convection Style Throughout Earth's History: From Stalled Plumes to Surface Dynamics
GEOCHEMISTRY, GEOPHYSICS, GEOSYSTEMS
08 february 2025
Ranpeng Li, Juliane Dannberg, Rene Gassmoeller, Ca...
Mineral phase transitions can either hinder or accelerate mantle flow. In the present day, the formation of the bridgmanite + ferropericl...
Plumes over LLSVPs: Supercharging multi-scale flow resolution with hybrid experimental-adjoint digital twins
INTERDISCIPLINARY PERSPECTIVES ON MANTLE FORMATION, STRUCTURE, AND DYNAMICS IN THE EARTH AND OTHER PLANETARY BODIES I POSTER
study of earth's deep interior | 12 december 2024
Xiyuan Bao, Carolina R. Lithgow-Bertelloni
Approximately half of global hotspots are significantly hotter than mid-ocean ridges, often exhibiting distinct geochemical signatures. These hotspots...
View Abstract
How Phase Transitions Impact Convection Style, Material Exchange, and Surface Dynamics throughout Earth’s History: A Modeling Study
REDISCOVERING EARTH’S MANTLE HETEROGENEITIES THROUGH IMAGING, MODELING, GEOCHEMISTRY, AND MINERAL EXPERIMENTS III ELIGHTNING
study of earth's deep interior | 12 december 2024
Ranpeng Li, Juliane Dannberg, Rene Gassmoeller, Ca...
Mineral phase transitions can either hinder or accelerate mantle flow. In the present day, the formation of the bridgmanite + ferropericlase assemblag...
View Abstract
Temporal variations in paleoshorelines from the evolution of subduction heterogeneity since the Paleozoic
ADVANCES IN DEEP EARTH–SURFACE INTERACTIONS I POSTER
study of earth's deep interior | 11 december 2024
Matthew Bogumil, Carolina R. Lithgow-Bertelloni
Subduction of oceanic plates represents the return of Earths top thermal boundary layer to the mantle, recycling both thermal and compositional hetero...
View Abstract
Role of Fault-Induced Rock Damage in Erosional Processes: A Global Analysis
THE EARTH'S SURFACE AS A NATURAL LAB: ADVANCES IN ISOLATING LANDSCAPE EVOLUTION CONTROLS III ELIGHTNING
earth and planetary surface processes | 11 december 2024
Boontigan Kuhasubpasin, Seulgi Moon, Carolina R. L...
Active faults significantly influence landscape morphology by tectonic and erosional processes. These faults drive surface movementsuplift, subsidence...
View Abstract
Earth's water content constrained by land exposure
PLANETARY HABITABILITY AND THE ROLE OF FLUIDS, MELTS, AND VOLATILES IN THE EVOLUTION OF TERRESTRIAL AND EXTRATERRESTRIAL PLANETARY SYSTEMS II ORAL
volcanology, geochemistry and petrology | 11 december 2024
Carolina R. Lithgow-Bertelloni, John P. Brodholt, ...
The content and evolution of the water content in Earths mantle have important implications for its internal dynamics and surface habitability. Water ...
View Abstract
Exploring the Connections between Subsurface Stress, Faults, and Rivers
TECTONIC AND GEODYNAMIC PROCESSES ENCODED IN LANDSCAPES I ORAL
earth and planetary surface processes | 10 december 2024
Seulgi Moon, Boontigan Kuhasubpasin, Carolina R. L...
The lithospheric stress field induces topography, faulting, and non-brittle deformation. At long wavelengths, these stress fields arise both from vari...
View Abstract
When do Plumes Merge? Quantifying controls on the timescale of mantle plume merger
OCEANIC MAGMATISM AND DYNAMICS: MULTIDISCIPLINARY PERSPECTIVES ON HOT SPOTS AND SEAMOUNTS I ELIGHTNING
volcanology, geochemistry and petrology | 09 december 2024
Joseph Lewis-Merrill, Carolina R. Lithgow-Bertello...
Hotspots have long been modeled as the surface expressions of thermo(-chemical) upwellings originating at the core-mantle boundary (CMB) dubbed mantle...
View Abstract