Michele L. Cooke
- ORCiD
- https://orcid.org/0000-0002-4407-9676
- OpenAlex ID
- https://openalex.org/A5009623213 (API record)
Associated Concepts [?]
- Geology
- Biology
- Paleontology
- Engineering
- Physics
- Seismology
- Thermodynamics
- Fault (geology)
- Aerospace engineering
- Tectonics
- Computer science
- Slip (aerodynamics)
- Mathematics
- Materials science
- Composite material
- Geography
- Quantum mechanics
- Geomorphology
- Structural basin
- Mechanical engineering
- Geometry
Authored Works
sorted by decreasing year, and then by display-name
- Why we need to crip the classroom (and the lab and the field...)
- The Effects of Pre-Stress Assumptions on Dynamic Rupture with Complex Fault Geometry in the San Gorgonio Pass, California, Region
- Predicting Off-fault Deformation Using Convolutional Neural Networks Trained On Experimental Strike-Slip Faults
- Loading Rate Influence on Restraining Bend Evolution
- From Classroom to Career: Building a Culture of Access for Geoscientists with Disabilities.
- A Kinematic and Morphometric Analysis of Restraining Bends in the Eastern California Shear Zone
- Prediction of Off-Fault Deformation from Experimental Strike-slip Fault Structures using the Convolutional Neural Networks
- Initiating new efforts to track and improve DEI within the Department of Geosciences at UMass Amherst
- 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?
Linked Co-Authors
- C. Kyriakopoulos
- Christine E. Hatch
- Cinzia Cervato
- D. D. Oglesby
- D. F. Boutt
- Elizabeth C Sibert
- Frances Griswold
- Hanna Elston
- Hannah Baranes
- Laura Wallace
- Roland Bürgmann
- Shaina Sadai
- V. Schulte-Pelkum
- Victor C. Tsai
- Whitney M. Behr
Linked Collaborating Institutions
- Brown University, Rhode Island
- Iowa State University
- Stanford University, California
- UMass Amherst
- University of California, Berkeley, Department of Earth and Planetary Science
- University of California, Riverside
- University of California, San Diego, Scripps Institution of Oceanography
- University of Colorado, Boulder
- University of Memphis, Tennessee
- University of South Florida
- University of Texas, Austin
- University of Texas, Austin, Department of Geological Sciences
- Virginia Polytechnic Institute and State University
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