CB
Member Since 2007
Carolyn J. Boulton
Lecturer, Victoria University of Wellington
AGU Research
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Heterogeneity in Microseismicity and Stress Near Rupture‐Limiting Section Boundaries Along the Late‐Interseismic Alpine Fault
JOURNAL OF GEOPHYSICAL RESEARCH: SOLID EARTH
08 october 2022
Emily Warren-Smith, John Townend, Calum J. Chamber...
Paleoseismic evidence from the late‐interseismic Alpine Fault suggests key section boundaries conditionally inhibit rupture. We utilize a yea...
Regional‐Scale Low‐Angle Normal Fault Friction and Cohesion Constrained From Mohr‐Coulomb Models of Active and Abandoned Range‐Front Faults in Papua New Guinea
JOURNAL OF GEOPHYSICAL RESEARCH: SOLID EARTH
20 april 2022
Samuel M. Webber, Timothy A. Little, Carolyn J. Bo...
Low‐angle normal faults (LANFs) are poorly understood, as their slip at <30° dips appears inconsistent with Byerlee friction and Ande...
Persistent compliance drives localization of deformation on a major plate boundary fault
MECHANICAL COMPLEXITY AND STRUCTURAL HETEROGENEITY IN DIFFUSE FAULT ZONES: OBSERVATION, MODELING, AND EXPERIMENTS II ORAL
seismology | 16 december 2021
Ludmila Adam, Shreya Kanakiya, Carolyn J. Boulton,...
The Alpine Fault is a major boundary between the Pacific and Australian plates in the South Island of New Zealand. The fault is late in its interseism...
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Characterizing the seismogenic potential of active faults in the Woodlark rift with integrated multi-timescale observations and models
PRE-, CO-, AND POST-RUPTURE PROCESSES ACROSS MULTIPLE SCALES III POSTER
mineral and rock physics | 15 december 2021
James Biemiller, Alice-Agnes Gabriel, Laura M. Wal...
Earthquakes in active rifts pose significant societal hazard, but identifying and characterizing seismically hazardous normal faults can be challengin...
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Using Syntectonic Calcite Veins to Reconstruct the Strength Evolution of an Active Low‐Angle Normal Fault, Woodlark Rift, SE Papua New Guinea
JOURNAL OF GEOPHYSICAL RESEARCH: SOLID EARTH
11 august 2021
Marcel Mizera, Timothy A. Little, Carolyn J. Boult...
Quantifying the strength evolution of faults that cut the lithosphere is essential to better understand seismicity in continental regions. We estim...
Unraveling the Slip Behavior and Evolution of the Mai’iu-Goodenough Detachment Fault System by Integrating Multi-timescale Datasets with Novel Coral Paleoseismological Evidence
INTEGRATING RELATED EARTHQUAKE DATA SETS: HOW TO COMBINE GEODESY, SEISMOLOGY, AND GEOLOGY IN INFORMATIVE WAYS I
tectonophysics | 16 december 2020
James Biemiller, Frederick W. Taylor, Luc Lavier, ...
Low-angle normal faults (LANFs; dip <30°) accommodate kilometers of crustal extension, but it remains unclear whether these faults can host large e...
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Slow‐to‐Fast Deformation in Mafic Fault Rocks on an Active Low‐Angle Normal Fault, Woodlark Rift, SE Papua New Guinea
GEOCHEMISTRY, GEOPHYSICS, GEOSYSTEMS
01 november 2020
Marcel Mizera, Timothy A. Little, Carolyn J. Boult...
Slip on the active Mai'iu low‐angle normal fault in Papua New Guinea that dips 15–24° at the surface has exhumed in its footwall a...
Mechanical Implications of Creep and Partial Coupling on the World's Fastest Slipping Low‐Angle Normal Fault in Southeastern Papua New Guinea
JOURNAL OF GEOPHYSICAL RESEARCH: SOLID EARTH
09 october 2020
James Biemiller, Carolyn J. Boulton, Laura M. Wall...
We use densely spaced campaign GPS observations and laboratory friction experiments on fault rocks from one of the world's most rapidly slipping lo...