Since the Industrial Revolution, anthropogenic carbon dioxide (CO2) emissions have grown
exponentially, accumulating in the atmosphere and leading to global warming. According to …

Carbon Dioxide removal from air (CDR) combined with permanent solid storage can be
accomplished via carbon mineralization in ultramafic rocks in at least four ways: 1. Surficial …

The rate of natural carbonation of tectonically exposed mantle peridotite during weathering
and low-temperature alteration can be enhanced to develop a significant sink for …

Near-surface reaction of CO2-bearing fluids with silicate minerals in peridotite and basalt
forms solid carbonate minerals. Such processes form abundant veins and travertine …

Carbon mineralization sequesters CO2 by reaction of alkaline earth metal bearing silicate
and hydroxide minerals with CO2 to form stable carbonate minerals. Seifritz (1990) …

Retrograde metamorphism (mineral hydration, carbonation and oxidation) is important in
controlling the composition and rheology of the Earth's crust and upper mantle, particularly …

Compressional intracontinental orogens are major zones of crustal thickening produced at
large distances from active plate boundaries. Consequently, any account of their initiation …

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 …

Extensive outcrops of listvenite—fully carbonated peridotite, with all Mg in carbonate
minerals and all Si in quartz—occur along the basal thrust of the Samail ophiolite in Oman …

A fundamental question in metamorphism is: What is the mechanism that converts one
mineral assemblage into another in response to a change in the physical and/or chemical …