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

Carbon storage through its mineralization in subsurface reactive basaltic and ultramafic
rocks offers the potential to safely store large quantities of CO 2 at a competitive price (eg …

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 …

Meter‐to hectometer‐size horizons of carbonate‐bearing talcschists are found along or near
the contacts between the different Liguro‐Piemont subduction slices. Through mineral and …

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 …

Mineral carbonation of mafic–ultramafic rocks has been highlighted as a promising way for
permanent carbon capture and storage. Carbonatization involves the release of Ca, Mg and …

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 …

Completely carbonated peridotites represent a window to study reactions of carbon‐rich
fluids with mantle rocks. Here, we present details on the carbonation history of listvenites …

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 …