Taca-Taca Alto porphyry copper deposit, province of Salta: Contributions to its knowledge

The Taca-Taca Alto porphyry copper deposit is located in western Puna, Salta Province, and is geneticaly related to an Oligocene volcanic sequence. Based on alteration-mineralization studies, three stages were recognized: 1. potasic alteration with magnetic-pyrrotite-pyrite-chalcopyrite-bornite-spha...

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Autores principales: Rubinstein, N., Segal, S., Zappettini, E.
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Acceso en línea:http://hdl.handle.net/20.500.12110/paper_00044822_v55_n1-2_p125_Rubinstein
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spelling todo:paper_00044822_v55_n1-2_p125_Rubinstein2023-10-03T13:57:32Z Taca-Taca Alto porphyry copper deposit, province of Salta: Contributions to its knowledge Rubinstein, N. Segal, S. Zappettini, E. Argentina Porphyry copper deposit Salta copper mineralization porphyry Argentina The Taca-Taca Alto porphyry copper deposit is located in western Puna, Salta Province, and is geneticaly related to an Oligocene volcanic sequence. Based on alteration-mineralization studies, three stages were recognized: 1. potasic alteration with magnetic-pyrrotite-pyrite-chalcopyrite-bornite-sphalerite and propylitic alteration with pyrite; 2. phyllic alteration with pyrite-molybdenite; 3. supergenic alteration mainly with limonite, jarosite, sericite, cuprite, alunite, digenite and covellite. In the area K/Ar dating shows that the volcanic sequence was emplaced during the Eocene-Oligocene and that hydrothermal alteration took place between 33.6 + -0.5 and 30.5 + -0.5 Ma. Therefore, it is possible to correlate the Taca-Taca Alto deposit with the Paleogene porphyry copper mineralization belt in Chile, suggesting a widening of the magmatic arc during the Oligocene at this latitude. JOUR info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by/2.5/ar http://hdl.handle.net/20.500.12110/paper_00044822_v55_n1-2_p125_Rubinstein
institution Universidad de Buenos Aires
institution_str I-28
repository_str R-134
collection Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA)
topic Argentina
Porphyry copper deposit
Salta
copper
mineralization
porphyry
Argentina
spellingShingle Argentina
Porphyry copper deposit
Salta
copper
mineralization
porphyry
Argentina
Rubinstein, N.
Segal, S.
Zappettini, E.
Taca-Taca Alto porphyry copper deposit, province of Salta: Contributions to its knowledge
topic_facet Argentina
Porphyry copper deposit
Salta
copper
mineralization
porphyry
Argentina
description The Taca-Taca Alto porphyry copper deposit is located in western Puna, Salta Province, and is geneticaly related to an Oligocene volcanic sequence. Based on alteration-mineralization studies, three stages were recognized: 1. potasic alteration with magnetic-pyrrotite-pyrite-chalcopyrite-bornite-sphalerite and propylitic alteration with pyrite; 2. phyllic alteration with pyrite-molybdenite; 3. supergenic alteration mainly with limonite, jarosite, sericite, cuprite, alunite, digenite and covellite. In the area K/Ar dating shows that the volcanic sequence was emplaced during the Eocene-Oligocene and that hydrothermal alteration took place between 33.6 + -0.5 and 30.5 + -0.5 Ma. Therefore, it is possible to correlate the Taca-Taca Alto deposit with the Paleogene porphyry copper mineralization belt in Chile, suggesting a widening of the magmatic arc during the Oligocene at this latitude.
format JOUR
author Rubinstein, N.
Segal, S.
Zappettini, E.
author_facet Rubinstein, N.
Segal, S.
Zappettini, E.
author_sort Rubinstein, N.
title Taca-Taca Alto porphyry copper deposit, province of Salta: Contributions to its knowledge
title_short Taca-Taca Alto porphyry copper deposit, province of Salta: Contributions to its knowledge
title_full Taca-Taca Alto porphyry copper deposit, province of Salta: Contributions to its knowledge
title_fullStr Taca-Taca Alto porphyry copper deposit, province of Salta: Contributions to its knowledge
title_full_unstemmed Taca-Taca Alto porphyry copper deposit, province of Salta: Contributions to its knowledge
title_sort taca-taca alto porphyry copper deposit, province of salta: contributions to its knowledge
url http://hdl.handle.net/20.500.12110/paper_00044822_v55_n1-2_p125_Rubinstein
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