Volcanic Sulfur Deposits in the Andes of Northern Chile (original) (raw)
Abstract
Native sulfur occurrences, which are very common in the Andes of northern Chile (18–28° S lat), are usually found directly related to summits, craters, and/or along flanks in almost all Upper Cenozoic volcanic edifices, mainly as sulfur mantos, breccias, veins, and amygdaloidal fillings. Other less common occurrences in these environments are sulfur flows, such as in the Lastarria volcano (Naranjo 1985).
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- Geostudios Ltda., Génova 2095, Santiago, Chile
F. Ferraris - Minera Anglo American Chile Ltda., Clasificador 31, Correo 9, Santiago, Chile
T. Vila
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- F. Ferraris
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- Département de Minéralogie, Université de Genève, 12, rue des Maraîchers, CH-1211, Genève 4, Switzerland
Lluís Fontboté - Mineralogisch-Petrographisches Institut, Universität Heidelberg, Im Neuenheimer Feld 236, D-6900, Heidelberg, Federal Republic of Germany
G. Christian Amstutz - Gerente de Exploraciones, Universidad Nacional de Ingeniería, and Newmont Peru Limited, Av. José Gálvez Barrenechea 218, Urb. Corpac, Lima-San Isidro, Peru
Miguel Cardozo - Facultad de Minas, Metalurgia y Geología, Universidad de Guanajuato, Ex-Hacienda de San Matías s/n, Apartado Postal 347, Guanajuato, Gto., 36020, Mexico
Esteban Cedillo - Programa de Geología Económica Aplicada, Universidad de Concepción, Casilla 4107, Concepción, Chile
José Frutos
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Ferraris, F., Vila, T. (1990). Volcanic Sulfur Deposits in the Andes of Northern Chile. In: Fontboté, L., Amstutz, G.C., Cardozo, M., Cedillo, E., Frutos, J. (eds) Stratabound Ore Deposits in the Andes. Special Publication No. 8 of the Society for Geology Applied to Mineral Deposits, vol 8. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-88282-1\_55
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