The Poopó polymetallic epithermal deposit, Bolivia: mineralogy, genetic constraints, and distribution of critical elements

dc.contributor.author Torres, Belén ca
dc.contributor.author Melgarejo, Joan Carles ca
dc.contributor.author Torró, Lisard ca
dc.contributor.author Camprubí, Antoni ca
dc.contributor.author Castillo-Oliver, Montgarri ca
dc.contributor.author Artiaga, David ca
dc.contributor.author Campeny, Marc ca
dc.contributor.author Tauler, Esperança ca
dc.contributor.author Jiménez-Franco, Abigail ca
dc.contributor.author Alfonso, Pura ca
dc.contributor.author Arce-Burgoa, Osvaldo R. ca
dc.contributor.other Consorci del Museu de Ciències Naturals de Barcelona ca
dc.date.accessioned 2025-11-05T13:06:08Z
dc.date.available 2025-11-05T13:06:08Z
dc.date.issued 2019-07-31
dc.description The tin-rich polymetallic epithermal deposit of Poopó, of plausible Late Miocene age, is part of the Bolivian Tin Belt. As an epithermal low sulfidation mineralisation, it represents a typological end-member within the “family” of Bolivian tin deposits. The emplacement of the mineralisation was controlled by the regional fault zone that constitutes the geological border between the Bolivian Altiplano and the Eastern Andes Cordillera. In addition to Sn and Ag, its economic interest resides in its potential in critical elements as In, Ga and Ge. This paper provides the first systematic characterisation of the complex mineralogy and mineral chemistry of the Poopó deposit with the twofold aim of identifying the mineral carriers of critical elements and endeavouring to ascertain plausible metallogenic processes for the formation of this deposit, by means of a multi-methodological approach. The poor development of hydrothermal alteration assemblage, the abundance of sulphosalts and the replacement of löllingite and pyrrhotite by arsenopyrite and pyrite, respectively, indicate that this deposit is ascribed to the low-sulphidation subtype of epithermal deposits, with excursions into higher states of sulphidation. Additionally, the occurrence of pyrophyllite and topaz has been interpreted as the result of discrete pulses of high-sulphidation magmatic fluids. The δ34SVCDT range in sulphides (−5.9 to −2.8‰) is compatible either with: (i) hybrid sulphur sources (i.e., magmatic and sedimentary or metasedimentary); or (ii) a sole magmatic source involving magmas that derived from partial melting of sedimentary rocks or underwent crustal assimilation. In their overall contents in critical elements (In, Ga and Ge), the key minerals in the Poopó deposit, based on their abundance in the deposit and compositions, are rhodostannite, franckeite, cassiterite, stannite and, less importantly, teallite, sphalerite and jamesonite. Keywords: critical elements; indium; gallium; germanium; tin; silver; low sulphidation; epithermal; Bolivian Tin Belt
dc.format application/pdf ca
dc.format.extent 25 p. ca
dc.identifier http://hdl.handle.net/2072/362205
dc.identifier https://doi.org/10.3390/min9080472
dc.identifier.citation Minerals 2019, 9(8), 472 ca
dc.identifier.entitat consorcis ca
dc.identifier.uri http://hdl.handle.net/11703/120661
dc.language eng ca
dc.provenance Recercat (Dipòsit de la Recerca de Catalunya) ca
dc.rights L'accés als continguts d'aquest document queda condicionat a l'acceptació de les condicions d'ús establertes per la següent llicència Creative Commons:http://creativecommons.org/licenses/by/4.0/
dc.rights.accessrights info:eu-repo/semantics/openAccess ca
dc.subject Bolívia
dc.subject Indi (Metall)
dc.subject Gal·li
dc.subject Germani
dc.subject Primeres matèries
dc.subject Jaciments minerals
dc.subject Estany
dc.subject 549
dc.subject.category Ciència i tecnologia ca
dc.subject.forma articles ca
dc.title The Poopó polymetallic epithermal deposit, Bolivia: mineralogy, genetic constraints, and distribution of critical elements
dc.type info:eu-repo/semantics/article
dc.type info:eu-repo/semantics/publishedVersion
dc.type.driver info:eu-repo/semantics/article ca
metadadalocal.dependencia 8008920

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