Victor C. Tsai
- ORCiD
- https://orcid.org/0000-0003-1809-6672
- OpenAlex ID
- https://openalex.org/A5087087014 (API record)
Associated Concepts [?]
- Geology
- Physics
- Biology
- Engineering
- Seismology
- Geography
- Computer science
- Paleontology
- Geomorphology
- Quantum mechanics
- Mathematics
- Optics
- Astronomy
- Oceanography
- Meteorology
- Artificial intelligence
- Geophysics
- Civil engineering
- Computer vision
- Telecommunications
- Acoustics
Authored Works
sorted by decreasing year, and then by display-name
- Towards the Geologic Parameterization of Seismic Tomography
- Seismic response of Nenana sedimentary basin, central Alaska
- Revisiting Global Temperature Calibrations for Lacustrine Branched GDGTs
- Monitoring Precipitation with a Dense Seismic Nodal Array
- Lake Stars as an Analog for Europa's Manannán Crater Spider Feature
- How is fault complexity linked to high-frequency radiation from Southern California earthquakes?
- What Controls the Frequency Dependence of Seismic Radiation Patterns? Insights from the LASSO Dense Array
- Rayleigh-Wave Ellipticity in Weakly Heterogeneous Layered Media
- Modeling P waves in seismic noise correlations: Application to fault monitoring using train traffic sources
- 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?
- Fault interactions enhance high-frequency earthquake radiation
- A Unified Model for Transient Subglacial Water Pressure and Basal Sliding
- A Nonlinear Model for Resolving the Temperature Bias of Branched Glycerol Dialkyl Glycerol Tetraether (brGDGT) Temperature Proxies
Linked Co-Authors
- A. Baltay
- Alex Gardner
- C. A. Dalton
- Carl Tape
- Daniel T. Trugman
- Erin Leonard
- Florent Brenguier
- Heiner Igel
- Hélène Seroussi
- J. David Neelin
- J. E. C. Scully
- Junlin Hua
- Korbinian Sager
- Kyle Smith
- L. C. Smith
- Laura Wallace
- Mark B. Bush
- Mathieu Choukroun
- Matthew M. Haney
- Mengxi Wu
- Meredith C. Parish
- Michele L. Cooke
- Pierre Boué
- R. Pappalardo
- Rachel E. Abercrombie
- Roland Bürgmann
- S. Diniega
- V. Schulte-Pelkum
- Whitney M. Behr
- Yixiao Sheng
Linked Collaborating Institutions
- Academia Sinica, Taiwan
- Boston University, Massachusetts
- Brown University, Rhode Island
- Chinese Academy of Sciences, Xian
- Dartmouth College, New Hampshire
- Florida Institute of Technology
- Jet Propulsion Laboratory
- Los Alamos National Laboratory, New Mexico
- Ludwig-Maximilians University of Munich, Germany
- UMass Amherst
- University of Alaska, Fairbanks
- University of California, Berkeley, Department of Earth and Planetary Science
- University of California, Los Angeles
- University of Colorado, Boulder
- University of Nevada, Reno
- University of North Dakota
- University of Texas, Austin
- University of Texas, Austin, Department of Geological Sciences
Add Incoming Edge
Login via ORCiD to contribute.
Add Outgoing Edge
Login via ORCiD to contribute.