Quantifying Non‐Thermal Silicate Weathering Using Ge/Si and Si Isotopes in Rivers Draining the Yellowstone Plateau Volcanic Field, USA

Abstract In active volcanic regions, high‐temperature chemical reactions in the hydrothermal system consume CO2 sourced from magma or from the deep crust, whereas reactions with silicates at shallow depths mainly consume atmospheric CO2. Numerous studies have quantified the load of dissolved solids...

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Autors principals:	François Gaspard, Sophie Opfergelt, Catherine Hirst, Shaul Hurwitz, R. Blaine McCleskey, Petra Zahajská, Daniel J. Conley, Pierre Delmelle
Format:	Artigo
Idioma:	Inglês
Publicat:	Wiley 2021-11-01
Col·lecció:	Geochemistry, Geophysics, Geosystems
Matèries:	Ge/Si silicon isotopes Yellowstone weathering hydrothermal seasonal
Accés en línia:	https://doi.org/10.1029/2021GC009904
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