Member Since 2007
Whitney M. Behr
Associate Professor, ETH Zurich Swiss Federal Institute of Technology Zurich
AGU Research
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GEOCHEMISTRY, GEOPHYSICS, GEOSYSTEMS
29 march 2025
Jacqueline E. Dixon, Paul D. Asimow, Whitney M. Be...
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Tracing packages of shallowly underplated sediments, Kenai, Alaska
SUBDUCTION TOP TO BOTTOM: CONVERGENT MARGIN PROCESSES TRENCH TO ARC (ALEUTIANS/ALASKA AND BEYOND) I ORAL
tectonophysics | 13 december 2024
Emily Hinshaw, Whitney M. Behr, Maria Fellin
The Valdez Group of the Chugach Terrane in Southern Alaska represents shallowly accreted sedimentary packages of flysch which were originally deposite...
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Insights from the Chugach accretionary complex in southern Alaska into underplating and exhumation processes and megathrust rheology at shallow subduction conditions
SUBDUCTION TOP TO BOTTOM: CONVERGENT MARGIN PROCESSES TRENCH TO ARC (ALEUTIANS/ALASKA AND BEYOND) III POSTER
tectonophysics | 13 december 2024
Whitney M. Behr, Ismay V. Akker, Luiz Morales, Mar...
The Chugach-Kodiak accretionary complex of southern Alaska extends over ~1200 km along strike and preserves structures formed during shallow subductio...
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Exploring the impact of plate velocity changes and channel rheology on exhumation within oceanic subduction models
SUBDUCTION ZONE ROCKS AND PROCESSES: FROM THE TRENCH TO THE SUBARC I POSTER
volcanology, geochemistry and petrology | 12 december 2024
Valeria Turino, Adam Holt, Derek J. Neuharth, Whit...
The dominant mechanisms behind the exhumation of high-pressure metamorphic crustal rocks in oceanic subduction settings are still highly debated. A fu...
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Characterizing quartz rheology through load-stepping experiments, from diffusion to dislocation creep
PHYSICAL PROPERTIES OF EARTH MATERIALS (PPEM): DEFORMATION, FLOW, AND FAILURE V POSTER
mineral and rock physics | 12 december 2024
Leif Tokle, Greg Hirth, Whitney M. Behr
Due to the abundance of quartz in the continental crust, quartz rheology is fundamental to our understanding of many geodynamic processes. Quartz rheo...
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Anatomy of a deep subduction megathrust at kilometric length scales: implications for slow slip and tremor
SLOW-TO-FAST EARTHQUAKES FROM SHALLOW TO DEEP: MULTISCALE RHEOLOGY OF PLATE BOUNDARY FAULTS II ORAL
seismology | 11 december 2024
Whitney M. Behr, Jesús Muñoz-Montecinos, Dominic H...
The deep sections of many modern subduction zones release strain through slow slip and tremor (SST), but the structures responsible, deformation mecha...
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Fluid‐Driven Shear Instabilities in the Subducted Oceanic Mantle at Intermediate Depths: Insights From Western Alps Meta‐Ophiolites
GEOCHEMISTRY, GEOPHYSICS, GEOSYSTEMS
24 august 2024
Jesús Munoz, Samuel Angiboust, Clothilde Minnaert,...
Serpentinites are major carriers of volatiles in deep subduction zones, releasing most fluids in the 500–650°C range. Despite fundamenta...
Structural Evolution, Exhumation Rates, and Rheology of the European Crust During Alpine Collision: Constraints From the Rotondo Granite—Gotthard Nappe
TECTONICS
21 june 2024
alberto ceccato, Whitney M. Behr, Alba Zappone, Lo...
The rheology of crystalline units controls the large‐scale deformation geometry and dynamics of collisional orogens. Defining a time‐co...