Tectonically driven carbonation of serpentinite by mantle CO2: Genesis of the Castiglioncello magnesite deposit in the Ligurian ophiolite of central Tuscany (Italy)-Reference-Cited by-同舟云学术

Tectonically driven carbonation of serpentinite by mantle CO2: Genesis of the Castiglioncello magnesite deposit in the Ligurian ophiolite of central Tuscany (Italy)

Published:2022-10 Issue: Volume:149 Page:105022
ISSN:0169-1368
Container-title:Ore Geology Reviews
language:en
Short-container-title:Ore Geology Reviews

Author:

Rielli Andrea,Boschi Chiara,Dini Andrea

Publisher

Elsevier BV

Subject

Economic Geology,Geochemistry and Petrology,Geology

Reference125 articles.

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4. Low Ni olivine in silica-undersaturated ultrapotassic igneous rocks as evidence for carbonate metasomatism in the mantle;Ammannati;Earth Planet. Sci. Lett.,2016

5. Stable isotope evidence for near-surface, low-temperature formation of Mg-(hydro) carbonates in highly altered Greek Mesozoic serpentinites;Andrews;J. Geol. Soc. London,2018

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