Atmospheric sulfur is recycled to the crystalline continental crust during supercontinent formation

The long-term evolution of the sulfur budget in the lithosphere is poorly constrained. Here, using mass independent isotope fractionation as an indelible tracer, the authors track the pathway of sulfur from the Earth’s surface to punctuated episodes of granitoid magmatism during collisional orogenes...

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Auteurs principaux: Crystal LaFlamme, Marco L. Fiorentini, Mark D. Lindsay, Thi Hao Bui
Format: article
Langue:EN
Publié: Nature Portfolio 2018
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Accès en ligne:https://doaj.org/article/0eb2699bb0024f38b2960fc3ef994b8d
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