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Ductile deformation of the lithospheric mantle
The strength of lithospheric plates is a central component of plate tectonics, governed by
brittle processes in the shallow portion of the plate and ductile behavior in the deeper …
brittle processes in the shallow portion of the plate and ductile behavior in the deeper …
Recent advances in characterizing the crustal stress field and future applications of stress data: perspectives from North America
JE Lundstern - 2024 - pubs.geoscienceworld.org
The stress field controls patterns of crustal deformation, including which faults are likeliest to
cause earthquakes or transmit fluids. Since the 1950s, maps of maximum horizontal stress …
cause earthquakes or transmit fluids. Since the 1950s, maps of maximum horizontal stress …
Deep hydration and lithospheric thinning at oceanic transform plate boundaries
Transform faults accommodate the lateral motions between lithospheric plates, producing
large earthquakes. Away from active transform boundaries, former oceanic transform faults …
large earthquakes. Away from active transform boundaries, former oceanic transform faults …
Constitutive behavior of rocks during the seismic cycle
S Barbot - AGU Advances, 2023 - Wiley Online Library
Establishing a constitutive law for fault friction is a crucial objective of earthquake science.
However, the complex frictional behavior of natural and synthetic gouges in laboratory …
However, the complex frictional behavior of natural and synthetic gouges in laboratory …
Pulse-like ruptures, seismic swarms, and tremorgenic slow-slip events with thermally activated friction
The evolution of frictional resistance on a fault affects the characteristics of seismic ruptures.
A wide range of rupture styles, from slow-slip events to fast earthquakes, can be explained …
A wide range of rupture styles, from slow-slip events to fast earthquakes, can be explained …
Fluid-assisted grain size reduction leads to strain localization in oceanic transform faults
Abstract Oceanic Transform Faults are major plate boundaries representing the most
seismogenic part of the mid ocean ridge system. Nonetheless, their structure and …
seismogenic part of the mid ocean ridge system. Nonetheless, their structure and …
A reciprocity‐based efficient method for improved source parameter estimation of submarine earthquakes with hybrid 3‐D teleseismic Green's functions
Accurate source parameters of global submarine earthquakes are essential for
understanding earthquake mechanics and tectonic dynamics. Previous studies have …
understanding earthquake mechanics and tectonic dynamics. Previous studies have …
Seismicity, fault architecture, and slip mode of the westernmost Gofar transform fault
Oceanic transform faults accommodate plate motions through both seismic and aseismic
slips. However, deformation partition and slip mode interaction at these faults remain elusive …
slips. However, deformation partition and slip mode interaction at these faults remain elusive …
Machine learning‐based new earthquake catalog illuminates on‐fault and off‐fault seismicity patterns at the Discovery Transform Fault, East Pacific Rise
Oceanic transform faults connect spreading centers and are imprinted with previous tectonic
events. However, their tectonic interactions are not well understood due to limited …
events. However, their tectonic interactions are not well understood due to limited …
Hydrous fluids down to the semi-brittle root zone of detachment faults in nearly amagmatic ultra-slow spreading ridges
At the Eastern part of the Southwest Indian Ridge (SWIR), plate divergence is
accommodated by large offset normal faults, also called detachment faults, that exhume …
accommodated by large offset normal faults, also called detachment faults, that exhume …