Section 9. In situ Mineral Carbonation of ultra mafic rocks
Year: 2012
Type: article
Abstract: Interaction between carbon bearing fluids and silicate minerals in mafic and ultramafic rocks during weathering or low grade metamorphism generally leads to the formation of carbonate minerals. The total consumption of carbon by silicate weathering alone has been estimated to be ∼150 Mt/year ([
Source: Geochemical Perspectives
Authors: Bjørn Jamtveit, Øyvind Hammer
Institution: University of Oslo
Language: English
Subfield: Environmental Engineering
Field: Environmental Science
Domain: Physical Sciences
SDG: Climate action
Open Access status: diamond
OpenAlex ID: W2336560315