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Geological fingerprints of deep slow earthquakes: A review of field constraints and directions for future research
Slow earthquakes, including low-frequency earthquakes, tremor, and geodetically detected
slow-slip events, have been widely detected, most commonly at depths of 40–60 km in …
slow-slip events, have been widely detected, most commonly at depths of 40–60 km in …
Dynamic slab segmentation due to brittle–ductile damage in the outer rise
Subduction is the major plate driving force, and the strength of the subducting plate controls
many aspects of the thermochemical evolution of Earth. Each subducting plate experiences …
many aspects of the thermochemical evolution of Earth. Each subducting plate experiences …
Criterion for residual strength and brittle-ductile transition of brittle rock under triaxial stress conditions
The critical condition with respect to the brittle-ductile transition (BDT) is of great significance
in understanding the distinction between brittle and ductile behavior for rocks. In this paper …
in understanding the distinction between brittle and ductile behavior for rocks. In this paper …
Brittle-ductile failure transition in geomaterials modeled by a modified phase-field method with a varying damage-driving energy coefficient
With elevated confining pressure and low temperatures, geomaterials may exhibit brittle-to-
ductile failure transition due to increased cataclastic flow. In this work, we propose a …
ductile failure transition due to increased cataclastic flow. In this work, we propose a …
[HTML][HTML] A comparison between rate-and-state friction and microphysical models, based on numerical simulations of fault slip
Rate-and-state friction (RSF) is commonly used for the characterisation of laboratory friction
experiments, such as velocity-step tests. However, the RSF framework provides little …
experiments, such as velocity-step tests. However, the RSF framework provides little …
A novel micromechanics-enhanced phase-field model for frictional damage and fracture of quasi-brittle geomaterials
Cracking in quasi-brittle geomaterials is a complex mechanical phenomenon, driven by
various dissipation mechanisms across multiple length scales. While some recent promising …
various dissipation mechanisms across multiple length scales. While some recent promising …
[HTML][HTML] Nanocrystalline principal slip zones and their role in controlling crustal fault rheology
Principal slip zones (PSZs) are narrow (< 10 cm) bands of localized shear deformation that
occur in the cores of upper-crustal fault zones where they accommodate the bulk of fault …
occur in the cores of upper-crustal fault zones where they accommodate the bulk of fault …
Semi‐brittle deformation of Carrara marble: Hardening and twinning induced plasticity
Semi‐brittle flow occurs when crystal plasticity and cataclastic mechanisms operate
concurrently and may be common at mid‐levels of the Earth's crust. Using a Paterson gas …
concurrently and may be common at mid‐levels of the Earth's crust. Using a Paterson gas …
Weak phases production and heat generation control fault friction during seismic slip
The triggering and magnitude of earthquakes is determined by the friction evolution along
faults. Experimental results have revealed a drastic decrease of the friction coefficient for …
faults. Experimental results have revealed a drastic decrease of the friction coefficient for …
Flow‐to‐friction transition in simulated calcite gouge: Experiments and microphysical modeling
A (micro) physical understanding of the transition from frictional sliding to plastic or viscous
flow has long been a challenge for earthquake cycle modeling. We have conducted ring …
flow has long been a challenge for earthquake cycle modeling. We have conducted ring …