Whitney M. Behr
- ORCiD
- https://orcid.org/0000-0002-3003-8670
- OpenAlex ID
- https://openalex.org/A5092120743 (API record)
Associated Concepts [?]
- Seismology
- Geology
- Tectonics
- Subduction
- Physics
- Petrology
- Paleontology
- Biology
- Zircon
- Thermodynamics
- Shear zone
- Nuclear physics
- Metamorphic rock
- Materials science
- Geochemistry
- Composite material
- Chemistry
- Membrane
- Lithosphere
- Grain boundary
- Genetics
- Crystallography
- Condensed matter physics
- Biochemistry
- Amphibole
Authored Works
sorted by decreasing year, and then by display-name
- Structural Mapping of the Eclogite Zone, Tauern Window: Implications for the rheology of the subduction zone interface
- Numerically Modelling Along-strike Rheologic Variations in 3D Subduction Zones
- Modeling Subduction Interface Shear Zone Seismic Anisotropy and Resulting Receiver Functions
- Metamorphism, Deformation, and Exhumation of the Blueschist-Greenschist Unit in Seldovia, Alaska
- Megathrust Deformation along Sediment-Rich- vs. Poor Subduction Margins - Examples from the Chugach Accretionary Prism, Alaska (USA)
- Influence of Solid-Fluid Interactions and Dilatancy on Seismic Cycles in a Poro-Visco-Elasto-Plastic Fault Structure
- Forearc Permeability and Fluid Flow in the Deep Slow Slip and Tremor Source Region: Insights From an Exhumed HP-LT Veined Sequence (Cycladic Blueschist, Greece)
- The influence of sediment accretion and transport on subduction zone dynamics.
- Seismic Signature of a Fossil Subduction Interface Shear Zone
- Past and Present Deformation along the San Andreas from Microseismicity, Geodesy, and Seismological Constraints
- Hydro-mechanical earthquake cycles in a poro-visco-elasto-plastic fluid-bearing fault
- Great unsolved questions in Tectonophysics: What is the role of inelastic off-fault deformation in the fault life cycle?
- Great Unsolved Questions in Tectonophysics: What physics governs fault networks? Can models make non-retrospective predictions that can be supported and/or falsified with near-future observations?
- Great Unsolved Questions in Tectonophysics: What is the Absolute Stress in the Lithosphere and Below?
- Great Unsolved Questions in Tectonophysics: What causes some faults to slip in major earthquakes, while others appear to creep and/or undergo episodic slow slip?
- Great Unsolved Questions in Tectonophysics: What are the transient rheologies of Earths lithosphere over the spectrum of deformation timescales, from milliseconds to tens of millions of years?
- Great Unsolved Questions in Tectonophysics: How do Lithospheric Layers and Asthenosphere Interact, and What are Their Rheological Properties as a Function of Depth?
- Experimental Investigation of Glaucophane Rheology Through General Shear Deformation Experiments
- Diffusion Creep of a Glaucophane-Bearing Blueschist
- Constraints from exhumed rocks on deep slow slip and tremor source processes and environment
Linked Co-Authors
- Betti Hegyi
- Carolyn M. Tewksbury-Christle
- Claudio Faccenna
- Debi Kilb
- Jesús Muñoz-Montecinos
- Laura Wallace
- Leif Tokle
- Lonnie Hufford
- Luca Dal Zilio
- Luiz F. G. Morales
- Meghan Miller
- Michele L. Cooke
- Miguel Cisneros
- Roland Bürgmann
- Silvia Brizzi
- T. W. Becker
- Taras Gerya
- V. Schulte-Pelkum
- Victor C. Tsai
- Ylona van Dinther
Linked Collaborating Institutions
- Australian National University, Canberra
- Brown University, Rhode Island
- California Institute of Technology
- ETH Zurich, Institute of Geophysics
- Eidgenossische Technische Hochschule, Zurich, Switzerland
- Lawrence Livermore National Laboratory, California
- Roma Tre University, Italy
- UMass Amherst
- University of California, Berkeley, Department of Earth and Planetary Science
- University of California, San Diego, Scripps Institution of Oceanography
- University of Colorado, Boulder
- University of Miami, Florida
- University of Northern British Columbia, Canada
- University of Texas, Austin
- University of Texas, Austin, Department of Geological Sciences
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