Member Since 2002
Christie D. Rowe
Director, University of Nevada, Reno
AGU Research
Search

Filters
Clear All
Field Evidence of Coseismic Pore Pressure Spikes from the Muddy Mountain Thrust, Southern Nevada, USA
SHALLOW FAULT ZONE DEFORMATION OVER THE EARTHQUAKE CYCLE: OBSERVATIONS, EXPERIMENTS, AND MODELS II ORAL
tectonophysics | 12 december 2024
Moses Angombe, Christie D. Rowe, Kiera Hamel, Maud...
High pore pressure in faults is often invoked as a weakening mechanism needed for fault slip, earthquake triggering, heat transport, fluid, and chemic...
View Abstract
Carbonation of Serpentinite in the San Andreas Fault Drives a Transition from Creeping to Locked Slip Behaviour
TECTONIC SETTINGS AND EARTHQUAKE POTENTIAL OF STRIKE-SLIP FAULT ZONES II ORAL
tectonophysics | 11 december 2024
Matthew Tarling, Christie D. Rowe
Several strands of the northern San Andreas Fault are creeping, and the creeping sections have often been linked to the presence of serpentinite rock ...
View Abstract
The Nevada Seismological Laboratory – Improving Seismic Network Operations within a Multi-Hazard Monitoring Operation
EARTHQUAKE MONITORING AND BEYOND IV POSTER
seismology | 10 december 2024
Kyren R. Bogolub, William H. Savran, Daniel T. Tru...
The Nevada Seismological Laboratory (NSL) built a statewide, microwave network through seismic monitoring, largely funded by the US Geological Survey ...
View Abstract
Localization and Delocalization During Seismic Slip
GEOPHYSICAL RESEARCH LETTERS
23 november 2024
Heather M. Savage, Christie D. Rowe

The thickness of a seismic slip layer controls style and rate of rupture propagation, frictional heating, weakening, and energy budget of earthquak...

View Publication
Architecture and Composition of the San Andreas Fault in Tomales Bay, Northern California
CONTROL OF FAULT ZONE HETEROGENEITY AND FAULT ROUGHNESS ON MULTISCALE DEFORMATION AT INTER- AND INTRAPLATE FAULT ZONES I ORAL
tectonophysics | 13 december 2023
Matthew Tarling, Christie D. Rowe, Erin Eves, Vero...
The northern San Andreas Fault at Tomales Bay is expressed as a linear inlet ~20 km long and ~0.72 km wide, where the fault is thought to consist of a...
View Abstract
Localization and delocalization during earthquakes
BRIDGING FIELD AND LABORATORY STUDIES TO UNVEIL THE MECHANISMS OF UNSTABLE FAULT SLIP I ORAL
tectonophysics | 12 december 2023
Christie D. Rowe, Heather M. Savage
Slipping zone thickness controls everything about earthquakes, from nucleation to propagation to the cessation of slip and post-seismic healing. Local...
View Abstract
Shaping the future with Seismica: building a sustainable diamond open access researcher-run journal
SEISMOLOGY GENERAL CONTRIBUTION: MISCELLANEOUS I POSTER
seismology | 11 december 2023
Samantha Teplitzky, Jaime Convers, Gareth Funning,...
Seismica, a new Diamond Open Access journal in Seismology and Earthquake Science, launched in July 2022. One year into production, we have received 90...
View Abstract
An Ongoing Search for Active Faults in the Western Quebec Seismic Zone, Eastern Canada
STRUCTURE, TECTONICS, AND SEISMICITY OF CRATONS I POSTER
tectonophysics | 11 december 2023
Aube Gourdeau, Veronica Prush, Christie D. Rowe, K...
The Western Québec Seismic Zone (WQSZ) is an intracratonic seismic zonewith historical damaging earthquakes (e.g. 1732 M5.8 Montréal, 1663 M7Charlevoi...
View Abstract