Member Since 1981
Martha K. Savage
Professor, Victoria University of Wellington
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Time Varying Crustal Anisotropy at Whakaari/White Island Volcano
GEOPHYSICAL RESEARCH LETTERS
08 june 2024
Dagim Yoseph Mengesha, Martha K. Savage, Arthur Jo...
Whakaari/White Island has been the most active New Zealand volcano in the 21st century, producing small phreatic and phreatomagmatic eruptions, whi...
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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Bulk Elastic Anisotropy of the Damage Zone of the Alpine Fault, South Island, New Zealand, from Combined DAS/Geophone Borehole Seismic Travel-time Tomography
BRIDGING FIELD AND LABORATORY STUDIES TO UNVEIL THE MECHANISMS OF UNSTABLE FAULT SLIP II POSTER
tectonophysics | 13 december 2023
Oumeng Zhang, Douglas R. Schmitt, Vera Lay, Stefan...
The damage zones of major faults influence initiation and propagation of earthquakes, fluid flows within the crust, and the long-term evolution of fau...
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Seismic Studies of Taupō Supervolcano, New Zealand: Seismicity, Apparent Tremor, Anisotropy and Imaging of a Magmatic Body Under the Auspices of the ECLIPSE Programme (Eruption or Catastrophe: Learning to Implement Preparedness for future Supervolcano Eruptions)
GEOPHYSICAL IMAGING OF MAGMA STORAGE AND TRANSPORT AT VOLCANOES III ORAL
volcanology, geochemistry and petrology | 13 december 2023
Martha K. Savage, Eleanor R H Mestel, Finnigan Ill...
We present the results of seismic studies from a five-year project to study Taupō volcano, including a deployment of 12 temporary seismometers (Octobe...
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Using Deep Learning Algorithms to Create a Microseismicity Catalogue of the Central Hikurangi Margin to Understand SSE Episodicity
SLOW-TO-FAST EARTHQUAKES FROM SHALLOW TO DEEP: OBSERVATIONS, EXPERIMENTS, AND NUMERICAL MODELING IV POSTER
tectonophysics | 13 december 2023
Stephen Kwong, Martha K. Savage, Emily Warren-Smit...
Slow slip events (SSEs) occur every ~5 years in the Pōrangahau region on the Central Hikurangi Margin. However, the permanent seismic instrumentation ...
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Fault re-activation in an inversion tectonic region, northwestern South Island, New Zealand.
EARTHQUAKE SOURCE CHARACTERIZATION AND FAULT ZONE PROPERTIES FROM MICROMETER TO KILOMETER SCALES IV POSTER
seismology | 12 december 2023
Ayaka Tagami, Miu Matsuno, Tomomi Okada, Martha K....
Introduction In New Zealand, the Pacific plate is subducting beneath the Australian plate in the North Island and the north part of the South Island. ...
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ANISOTROPY CHANGES BEFORE AND AFTER THE ERUPTION OF WHAKAARI/WHITE ISLAND VOLCANO, NEW ZEALAND
OCEAN ISLAND VOLCANOES: FROM QUIESCENCE THROUGH ERUPTION II POSTER
volcanology, geochemistry and petrology | 12 december 2023
Dagim Yoseph Mengesha, Martha K. Savage, Arthur Jo...
Whakaari/White Island has been the most active New Zealand volcano in the 21st century, producing small phreatic and phreatomagmatic eruptions, which ...
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Seismic imaging of the Noto Peninsula earthquake swarm in Japan using temporal seismic stations
PHYSICAL CONTROLS OF EARTHQUAKE SWARM EVOLUTION I POSTER
seismology | 11 december 2023
Tomomi Okada, Martha K. Savage, Shin'ichi Sakai, K...
In this study, we examined the seismic wave velocity structure in the source region of an earthquake swarm in the Noto Peninsula, Ishikawa Prefecture,...
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