Mineralogy and distribution of critical elements in the Sn–W–Pb–Ag–Zn Huanuni Deposit, Bolivia

dc.contributor.author Cacho, Andreu ca
dc.contributor.author Melgarejo, Joan Carles ca
dc.contributor.author Camprubí, Antoni ca
dc.contributor.author Torró, Lisard ca
dc.contributor.author Castillo-Oliver, Montgarri ca
dc.contributor.author Torres, Belén ca
dc.contributor.author Artiaga, David ca
dc.contributor.author Tauler, Esperança ca
dc.contributor.author Martínez, Álvaro ca
dc.contributor.author Campeny, Marc 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.coverage.spatial Bolívia ca
dc.date.accessioned 2025-11-05T13:06:05Z
dc.date.available 2025-11-05T13:06:05Z
dc.date.issued 2019-12-04
dc.description The polymetallic Huanuni deposit, a world-class tin deposit, is part of the Bolivian tin belt. As a likely case for a “mesothermal” or transitional deposit between epithermal and porphyry Sn types (or shallow porphyry Sn), it represents a case that contributes significantly to the systematic study of the distribution of critical elements within the “family” of Bolivian tin deposits. In addition to Sn, Zn and Ag, further economic interest in the area resides in its potential in critical elements such as In, Ga and Ge. This paper provides the first systematic characterisation of the complex mineralogy and mineral chemistry of the Huanuni deposit with the twofold aim of identifying the mineral carriers of critical elements and endeavouring plausible metallogenic processes for the formation of this deposit, by means of a multi-methodological approach. With In concentrations consistently over 2000 ppm, the highest potential for relevant concentrations in this metal resides in widespread tin minerals (cassiterite and stannite) and sphalerite. Hypogene alteration assemblages are hardly developed due to the metasedimentary nature of host rocks, but the occurrence of potassium feldspar, schorl, pyrophyllite and dickite as vein material stand for potassic to phyllic or advanced argillic alteration assemblages and relatively high-temperature (and low pH) mineralising fluids. District-scale mineralogical zonation suggests a thermal zonation with decreasing temperatures from the central to the peripheral areas. A district-scale zonation has been also determined for δ34SVCDT values, which range −7.2‰ to 0.2‰ (mostly −7‰ to −5‰) in the central area and −4.2‰ to 1.0‰ (mainly constrained between −2‰ and 1‰) in peripheral areas. Such values stand for magmatic and metasedimentary sources for sulfur, and their spatial zoning may be related to differential reactivity between mineralising fluids and host rocks, outwardly decreasing from the central to the peripheral areas. Keywords: critical elements; indium; gallium; germanium; tin; silver; cerium; hydrothermal; bolivian tin belt
dc.format application/pdf ca
dc.format.extent 26 p. ca
dc.identifier http://hdl.handle.net/2072/366483
dc.identifier https://doi.org/10.3390/min9120753
dc.identifier.citation Minerals 2019, 9, 753 ca
dc.identifier.entitat consorcis ca
dc.identifier.uri http://hdl.handle.net/11703/120663
dc.language eng ca
dc.provenance Recercat (Dipòsit de la Recerca de Catalunya) ca
dc.publisher MDPI 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 Estany ca
dc.subject Indi (Metall) ca
dc.subject Gal·li ca
dc.subject Germani ca
dc.subject Jaciments minerals ca
dc.subject.category Ciència i tecnologia ca
dc.subject.forma articles ca
dc.title Mineralogy and distribution of critical elements in the Sn–W–Pb–Ag–Zn Huanuni Deposit, Bolivia
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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