HelioWebLaura Wallace
flowchart
A[Laura Wallace]
AC["Associated Concepts (22)"]
AW["Authored Works (9)"]
CA["Linked Co-Authors (24)"]
CI["Linked Collaborating Institutions (21)"]
A== dcterms:relation ==>AC
AW== author ==>A
AW== author ==>CA
AW== affil ==>CI
click AC "#associated-concepts"
click AW "#authored-works"
click CA "#co-authors"
click CI "#collaborating-institutions"
NI["add incoming edge"]
NO["add outgoing edge"]
NI-- ? -->A
A-- ? -->NO
click NI "#add-incoming-edge"
click NO "#add-outgoing-edge"
style NI stroke-width:2px,stroke-dasharray: 5 5
style NO stroke-width:2px,stroke-dasharray: 5 5
- ORCiD
- https://orcid.org/0000-0003-2070-0891
- OpenAlex ID
- https://openalex.org/A5052652649 (API record)
Associated Concepts [?]
- Geology
- Biology
- Seismology
- Paleontology
- Engineering
- Physics
- Tectonics
- Subduction
- Aerospace engineering
- Thermodynamics
- Geography
- Slip (aerodynamics)
- Oceanography
- Computer science
- Materials science
- Episodic tremor and slip
- Composite material
- Geodesy
- Mathematics
- Geophysics
- Geochemistry
- Civil engineering
Authored Works
sorted by decreasing year, and then by display-name
- The significance of vertical land movements at convergent plate boundaries in probabilistic sea-level projections for AR6 scenarios: The New Zealand case.
- Insights into the occurrence and characteristics of near-trench slow slip events at the central Hikurangi subduction zone from a recent seafloor geodetic experiment
- Fluids Circulation in Subduction Zones: How Fluids Impact Seismic/Aseismic Slip in Ecuador ?
- Near-field observations of shallow slow slip events revealed by IODP observatories at the Hikurangi subduction zone
- 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 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?
- Assessing the interplay between deep subduction interface slow slip events and large local earthquakes at the Hikurangi subduction zone, New Zealand
Linked Co-Authors
- A. Galvé
- C. A. Williams
- D. M. Saffer
- Emily Warren‐Smith
- I. J. Hamling
- Jérôme Lebrun
- Kimihiro Mochizuki
- M. Paulatto
- Martha K. Savage
- Michele L. Cooke
- Nicholas R. Golledge
- Nicola Litchfield
- Paul Denys
- R. H. Levy
- Robert Kopp
- Roland Bürgmann
- Ryota Hino
- Sigrún Hreinsdóttir
- T. Naish
- V. Schulte-Pelkum
- Victor C. Tsai
- Whitney M. Behr
- Yoshihiro Ito
- Yusuke Yamashita
Linked Collaborating Institutions
- Brown University, Rhode Island
- Geological Survey of Canada Pacific
- Geological and Nuclear Science Ltd, New Zealand
- IFREMER, Centre de Bretagne
- Karlsruhe Institute of Technology, Germany
- Kyoto University, Disaster Prevention Research Institute
- Kyushu University, Japan
- National Institute of Water and Atmospheric Research, New Zealand
- Observatoire de la Cote d'Azur, France
- Rutgers University, Department of Earth and Planetary Sciences
- Rutgers University, New Jersey
- Tohoku University, Japan
- UMass Amherst
- Universite de Rennes 1, CAESS Geosciences
- University of California, Berkeley, Department of Earth and Planetary Science
- University of Otago, New Zealand
- University of Oxford, UK
- University of Texas, Austin
- University of Texas, Austin, Department of Geological Sciences
- University of Tokyo, Japan
- Victoria University of Wellington, New Zealand
Add Incoming Edge
Login via ORCiD to contribute.
Add Outgoing Edge
Login via ORCiD to contribute.