ChambefortI, DillesJH, KentAJR.2008. Anhydrite-bearing andesite and dacite as a source for sulfur in magmatic-hydrothermal mineral deposits.Geology. 36(9):719–722. doi:10.1130/G24920A.1.
2.
DillesJH, KentAJR, WoodenJL, TosdalRM, KoleszarA, LeeRG, FarmerLP.2015. Zircon compositional evidence for sulfur-degassing from ore-forming arc magmas.Econ Geol. 110(1):241–251. doi:10.2113/econgeo.110.1.241.
3.
GustafsonLB, HuntJP.1975. The porphyry copper deposit at El Salvador, Chile.Econ Geol. 70(5):857–912. doi:10.2113/gsecongeo.70.5.857.
4.
JugoPJ, LuthRW, RichardsJP.2005. An experimental study of the sulfur content in basaltic melts saturated with immiscible sulfide or sulfate liquids at 1300°C and 10 GPa.J Petrol. 46(4):783–798. doi:10.1093/petrology/egh097.
5.
LuhrJF.1990. Experimental phase relations of water-and sulfur-saturated arc magmas and the 1982 eruptions of El Chichón volcano.J Petrol. 31(5):1071–1114. doi: 10.1093/petrology/31.5.1071
6.
MatthewsSJ, SparksRSJ, GardewegMC.1999. The Piedras Grandes–Soncor eruptions, lascar volcano, Chile; evolution of a zoned magma chamber in the central Andean upper crust.J Petrol. 40(12):1891–1919. doi:10.1093/petroj/40.12.1891.