Slab dehydration in warm subduction zones at depths of episodic slip and tremor
Non-volcanic tremor (NVT) and episodic slow slip events (SSEs) have been observed below
the seismogenic zone of relatively warm subduction zones for the past 20 years …
the seismogenic zone of relatively warm subduction zones for the past 20 years …
[HTML][HTML] Fluid flow in the subduction channel: Tremolite veins and associated blackwalls in antigoritite (Villa Clara serpentinite mélange, Cuba)
L Butjosa, A Cambeses, JA Proenza… - Lithos, 2023 - Elsevier
Exotic blocks of massive antigorite-serpentinite (antigoritite) document a deep-seated
subduction channel in the Villa Clara serpentinite-matrix mélange, central Cuba. The …
subduction channel in the Villa Clara serpentinite-matrix mélange, central Cuba. The …
Metasomatism at a metapelite–ultramafic rock contact at the subduction interface: Insights into mass transfer and fluid flow at the mantle wedge corner
Metasomatism of the subducting slab and mantle wedge influences the rheological and
chemical properties of rocks at the subduction zone interface. We investigated a serpentinite …
chemical properties of rocks at the subduction zone interface. We investigated a serpentinite …
[HTML][HTML] Effect of normal stress on the frictional behavior of brucite: application to slow earthquakes at the subduction plate interface in the mantle wedge
We report the results of friction experiments on brucite under both dry and wet conditions
under various normal stresses (10–60 MPa). The final friction coefficients of brucite were …
under various normal stresses (10–60 MPa). The final friction coefficients of brucite were …
Effect of normal stress on the friction of brucite: Application to slow earthquake in the mantle wedge
We report the results of friction experiments on brucite under both dry and water-saturated
(wet) conditions under various normal stresses (10–60 MPa). The steady-state friction …
(wet) conditions under various normal stresses (10–60 MPa). The steady-state friction …