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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 …
Sulfur disproportionation in deep COHS slab fluids drives mantle wedge oxidation
Sulfur degassed at volcanic arcs calls for dissolved sulfate ions (S6+) released by
subduction-zone fluids, oxidizing (in association with carbon) the subarc mantle, but sulfur …
subduction-zone fluids, oxidizing (in association with carbon) the subarc mantle, but sulfur …
Fault‐valve instability: A mechanism for slow slip events
Geophysical and geological studies provide evidence for cyclic changes in fault‐zone pore
fluid pressure that synchronize with or at least modulate slip events. A hypothesized …
fluid pressure that synchronize with or at least modulate slip events. A hypothesized …
Fluid‐driven shear instabilities in the subducted oceanic mantle at intermediate depths: Insights from Western Alps meta‐ophiolites
Serpentinites are major carriers of volatiles in deep subduction zones, releasing most fluids
in the 500–650° C range. Despite fundamental implications for mass transfer and …
in the 500–650° C range. Despite fundamental implications for mass transfer and …
Laboratory hydrofractures as analogs to tectonic tremors
The fracture of Earth materials occurs over a wide range of time and length scales. Physical
conditions, particularly the stress field and Earth material properties, may condition rupture …
conditions, particularly the stress field and Earth material properties, may condition rupture …
[HTML][HTML] Omphacitite formation and fluid-rock interaction processes in an intra-slab eclogite-facies shear zone
We document the formation of omphacitites in the Monviso Lago Superiore Unit (W. Alps)
where eclogite-facies, serpentinite-bearing shear zones host ample evidence for intense …
where eclogite-facies, serpentinite-bearing shear zones host ample evidence for intense …
[HTML][HTML] In situ rubidium–strontium geochronology of white mica in young metamafic and metasomatic rocks from Syros: testing the limits of laser-ablation triple …
The recent development of laser-ablation triple-quadrupole inductively coupled plasma
mass spectrometry (LA-ICP-MS/MS) has revolutionized rubidium–strontium (Rb–Sr) mica …
mass spectrometry (LA-ICP-MS/MS) has revolutionized rubidium–strontium (Rb–Sr) mica …
[HTML][HTML] Mesoscale fractures control the scale dependences of seismic velocity and fluid flow in subduction zones
Natural geological systems contain porosity structures of various scales that play different
roles in geophysical properties, fluid flow, and geodynamics. To understand seismic activity …
roles in geophysical properties, fluid flow, and geodynamics. To understand seismic activity …
In-situ Rb-Sr geochronology of white mica in young metamafic and metasomatic rocks from Syros: testing the limits of LA-ICP-MS/MS mica dating using different …
The recent development of LA-ICP-MS/MS has revolutionized Rb-Sr mica dating allowing to
obtain isotopic data within their microstructural context. While effective for old and felsic …
obtain isotopic data within their microstructural context. While effective for old and felsic …
On Fluid-Metamorphic Regime of Deep Fault Zones, in Connection with “Topical Issues in Hydrogeology of Seismogenic Fault Zones” by GG Kocharyan and IV …
MV Rodkin - Izvestiya, Physics of the Solid Earth, 2024 - Springer
In many aspects, the deep fluid regime plays a key role in seismicity, aseismic deformation
of the lithosphere, and ore and oil genesis processes. An informative detailed analysis of the …
of the lithosphere, and ore and oil genesis processes. An informative detailed analysis of the …