Abstract: <i>Non-zero ∆<sup>33</sup>S preserved in rocks from the Basal Ultramafic Sequence indicate crustal contamination in the most primitive magma of the Rustenburg Layered Suite (Bushveld Complex, South Africa)</i> (2017 AGU Fall Meeting)

Non-zero ∆³³S preserved in rocks from the Basal Ultramafic Sequence indicate crustal contamination in the most primitive magma of the Rustenburg Layered Suite (Bushveld Complex, South Africa)

Nivea Magalhaes¹, Allan Wilson², Sarah Penniston-Dorland³ and James Farquhar¹, (1)University of Maryland College Park, College Park, MD, United States, (2)University of the Witwatersrand, Johannesburg, South Africa, (3)University of Maryland College Park, Department of Geology, College Park, MD, United States

Back to: Volatiles in Terrestrial Planets: Their Role and Signatures in Differentiation, Volcanic, Magmatic, and Atmospheric Processes II Posters

Non-zero ∆33S preserved in rocks from the Basal Ultramafic Sequence indicate crustal contamination in the most primitive magma of the Rustenburg Layered Suite (Bushveld Complex, South Africa)

Non-zero ∆³³S preserved in rocks from the Basal Ultramafic Sequence indicate crustal contamination in the most primitive magma of the Rustenburg Layered Suite (Bushveld Complex, South Africa)