Raman spectroscopy to determine CO2 solubility in mafic silicate melts at high pressure: Haplobasaltic, haploandesitic and approach of basaltic compositions

Autor: Nicolas Sator, Julien Amalberti, Philippe Sarda, Daniel R. Neuville, Charles Le Losq, Bertrand Guillot, Tahar Hammouda, Sylvie Le Floch, Eva Chamorro-Pérez

Publikováno v: Chemical Geology
Chemical Geology, 2021, 582, pp.120413. ⟨10.1016/j.chemgeo.2021.120413⟩
Chemical Geology, Elsevier, 2021, 582, pp.120413. ⟨10.1016/j.chemgeo.2021.120413⟩

CO2 degassing of mafic silicate melts is an important part of the terrestrial carbon cycle, at mid-ocean ridges, oceanic hot spots, or in the middle of continents. Deeper CO2-bearing mafic magmas may also exist, such as those suspected in the D″ zo

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https://univ-lyon1.hal.science/hal-03325013