Carbonation of ultramafic rocks is a key piece of the global carbon cycle taking place from
the seafloor to the surficial environment and becoming particularly efficient in the genesis of …

Pore fluid pressure on subduction zone megathrusts is lowered by fluid drainage into the
overlying plate, affecting subduction zone seismicity. However, the spatial and temporal …

Listvenites form by metasomatic transformation of variably serpentinized peridotites to
carbonate-quartz rocks due to extensive reaction with CO 2-bearing aqueous fluids. This …

A model for intermediate-depth earthquakes of subduction zones is evaluated based on
shear localization, shear heating, and runaway creep within thin carbonate layers in an …

This paper provides an overview of research on core from Oman Drilling Project Hole BT1B
and the surrounding area, plus new data and calculations, constraining processes in the …

In subduction zones, carbon from the surface can be transported into Earth's interior. Fluids
released during subduction can mobilize carbon bound in solid minerals in the subducting …

The serpentinized and tectonized mantle in the Decar area in central British Columbia,
including rocks that host the Baptiste Ni Deposit, consists of several ultramafic protolith …

In this paper, we present mineralogical, whole-rock geochemical, Sr and Pb isotopic, and
zircon trace elemental and U–Pb geochronological data for the newly-discovered Pengco …

Carbonated serpentinites (listvenites) in the Samail Ophiolite, Oman, record mineralization
of 1–2 Gt of CO2, but the mechanisms providing permeability for continued reactive fluid flow …

The ability to precisely constrain the physical–chemical conditions of serpentinization, such
as temperature and fluid source, is limited by the accuracy of calibrations for oxygen isotope …