LW
Member Since 1997
Laura M. Wallace
Professor, GEOMAR Helmholtz Centre for Ocean Research Kiel
AGU Research
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Low‐Frequency Earthquakes Downdip of Deep Slow Slip Beneath the North Island of New Zealand
JOURNAL OF GEOPHYSICAL RESEARCH: SOLID EARTH
10 may 2024
Florent Aden-Antoniów, William B. Frank, Calum J. ...
We report the first catalog of low‐frequency earthquakes in the Hikurangi subduction zone, located beneath the Kaimanawa Range of the North I...
Slow Slip Events in New Zealand: Irregular, yet Predictable?
GEOPHYSICAL RESEARCH LETTERS
15 march 2024
Sandro Truttmann, Thomas Poulet, Laura M. Wallace,...
Current earthquake forecasting approaches are mainly based on probabilistic assumptions, as earthquakes seem to occur randomly. Such apparent rando...
Inverting Geodetic Strain Rates for Slip Deficit Rate in Complex Deforming Zones: An Application to the New Zealand Plate Boundary
JOURNAL OF GEOPHYSICAL RESEARCH: SOLID EARTH
08 march 2024
Kaj M. Johnson, Laura M. Wallace, Jeremy Maurer, I...
The potential for future earthquakes on faults is often inferred from inversions of geodetically derived surface velocities for locking on faults u...
Observations of along-isobath correlation in seafloor pressure records from multiple margins in the Pacific
OCEAN SCIENCES 2024
physical oceanography: mesoscale and larger | 20 february 2024
Erik K. Fredrickson, Laura M. Wallace, William S. ...
In the past decade, efforts to observe solid-earth geophysical processes beneath the ocean have resulted in a number of temporary and permanent/cabled...
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Insights into the occurrence and characteristics of near-trench megathrust slip behavior at the Hikurangi subduction zone from almost a decade of seafloor geodetic experiments
RECENT APPLICATIONS AND DEVELOPMENTS IN SEAFLOOR GEODESY I ORAL
geodesy | 14 december 2023
Laura M. Wallace, Spahr C. Webb, John B. DeSanto, ...
Resolving the distribution of interseismic coupling and transient slow slip event (SSE) processes at offshore subduction zones is hampered by the diff...
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The evolution of fluid flow throughout the slow slip cycle: testing the hydrologic response to SSEs at the Hikurangi subduction zone
SUBDUCTION TOP TO BOTTOM (ST2B): THE NATURE OF THE SUBDUCTION INTERFACE, EARTHQUAKES, AND THE ROLES OF FLUIDS I POSTER
tectonophysics | 14 december 2023
Irita E. Aylward, Evan A. Solomon, Theresa L. Whor...
The balance of fluid inputs, storage, and drainage is thought to play a vital role in the nature and timing of fault slip at subduction zones. Further...
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Seafloor observations of a 2022 shallow slow slip event in the Hikurangi Subduction Zone offshore Gisborne
RECENT APPLICATIONS AND DEVELOPMENTS IN SEAFLOOR GEODESY II POSTER
geodesy | 14 december 2023
Erik K. Fredrickson, Laura M. Wallace, Yoshihiro I...
Slow slip events have been found to occur regularly in the offshore reaches of the Hikurangi Subduction Zone off New Zealands north island. Surface de...
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Strain Rate Mapping and Earthquake Hazard
STRAIN RATE MAPPING AND EARTHQUAKE HAZARD I ORAL
geodesy | 13 december 2023
Jeremy Maurer, Kaj M. Johnson, Laura M. Wallace, I...
Geodetic data in plate boundary zones reflect the accrual of tectonic strain and stress (much of which will ultimately be released in earthquakes), an...
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