dc.creatorNoble, Donald C.
dc.creatorNavarro Colque, Pedro Alexis
dc.creatorQuispesivana Quispe, Luis Juan
dc.creatorSpell, Terry
dc.date.accessioned2022-01-04T18:00:59Z
dc.date.accessioned2022-10-27T15:39:23Z
dc.date.available2022-01-04T18:00:59Z
dc.date.available2022-10-27T15:39:23Z
dc.date.created2022-01-04T18:00:59Z
dc.date.issued2002
dc.identifierNoble, D.; Navarro, P.; Quispesivana, L. & Spell, T. (2002) - Highly differentiated "Topaz" rhyolite in the high plateau province of southern Peru. En: Congreso Peruano de Geología, 11, Lima, 2002. Resúmenes. Lima: Sociedad Geológica del Perú, p. 203.
dc.identifierhttps://hdl.handle.net/20.500.12544/3568
dc.identifierXI Congreso Peruano de Geología, Lima, 25 – 28 septiembre 2002. Resúmenes.
dc.identifier.urihttps://repositorioslatinoamericanos.uchile.cl/handle/2250/4907756
dc.description.abstractHigh-silica rhyolite is present in various parts of southern Perú. Rhyolite from two localites, the Cailloma caldera and the newly recognized Río Chalhuanca dome field, both in Arequipa Department, belong to the group of "topaz" rhyolites well known in the eastern and central parts ofthe Great Basin and New Mexico, Western U.S., and in many localities in Mexico ( e.g., Christian sen et al., Geol. S oc. Am. Spec. Paper 205). The Peruvian occurrences may be the first topaz rhyolites recognized in South America.
dc.languagespa
dc.publisherSociedad Geológica del Perú
dc.publisherPE
dc.rightshttps://creativecommons.org/licenses/by-nc-nd/4.0/deed.es
dc.rightsinfo:eu-repo/semantics/openAccess
dc.sourceRepositorio Institucional INGEMMET
dc.sourceInstituto Geológico, Minero y Metalúrgico – INGEMMET
dc.subjectGeología económica
dc.subjectToba volcánica
dc.titleHighly differentiated "Topaz" rhyolite in the high plateau province of southern Peru
dc.typeActas de congresos


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