Mineral carbon storage in mafic and ultramafic rock masses has the potential to be an
effective and permanent mechanism to reduce anthropogenic CO2. Several successful pilot …

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

Chrysotile, the most common serpentine polymorph, represents one of the most hazardous
mine wastes known for its associated health risks. For the first time, chrysotile mine waste …

Basalt formations are promising candidates for the geologic storage of anthropogenic CO2
due to their storage capacity, porosity, permeability, and reactive geochemical trap** …

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 …

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 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 …

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 …

Volcanoes represent one of the most critical geological settings for hazard modelling due to
their propensity to both unpredictably erupt and collapse, even in times of quiescence …

Peridotites (olivine-rich rocks) naturally react with CO 2-rich fluids to eventually form
carbonates. Complete conversion involves incorporation of substantial amounts of CO 2 …