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Geology; June 1998; v. 26; no. 6; p. 523-526; DOI: 10.1130/0091-7613(1998)026<0523:SEOOAM>2.3.CO;2
© 1998 Geological Society of America
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Sulfur evolution of oxidized arc magmas as recorded in apatite from a porphyry copper batholith

Martin J. Streck1 and John H. Dilles1

1 Department of Geosciences, Oregon State University, Corvallis, Oregon 97331-5506

Uniformly sulfur-rich cores abruptly zoned to sulfur-poor rims (~1 to <0.2 wt% SO3) in apatite from the Yerington batholith, Nevada, indicate that early magma that is crystal poor, oxidizing, and sulfate rich evolved to sulfate-poor magma via crystallization of anhydrite, a mineral observed in magmas from Pinatubo and El Chichón. We predict that the characteristic zonation to sulfur-poor rims of apatite in the Yerington batholith is common in other oxidized, hydrous, calc-alkaline magmas, and can be used to track cryptic anhydrite saturation as well as to monitor sulfur evolution. Sulfate-rich arc magmas such as Yerington magmas may crystallize to produce hydrothermal fluids rich in chlorine, copper, and sulfur and porphyry copper ores.




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