Magnetic mineralogy of Variscan granites from northern Portugal: an approach to their petrogenesis and metallogenic potential

Northern Portugal is characterized by the occurrence of numerous W hydrothermal deposits spatially associated with granites. The primary goal of this work is to establish a relationship between the magnetic behavior of the granites and the redox conditions during magma genesis, as this can influenc...

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Main Authors: C. Cruz, H. Sant'Ovaia, F. Noronha
Format: Article
Language:English
Published: Universitat de Barcelona (UB), Geociències Barcelona (Geo3BCN), Institut de Diagnosi Ambiental i Estudis de l'Aigua (IDAEA), Universitat Autònoma de Barcelona (UAB) 2020-03-01
Series:Geologica Acta
Subjects:
Online Access:https://revistes.ub.edu/index.php/GEOACTA/article/view/28718
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author C. Cruz
H. Sant'Ovaia
F. Noronha
author_facet C. Cruz
H. Sant'Ovaia
F. Noronha
author_sort C. Cruz
collection DOAJ
description Northern Portugal is characterized by the occurrence of numerous W hydrothermal deposits spatially associated with granites. The primary goal of this work is to establish a relationship between the magnetic behavior of the granites and the redox conditions during magma genesis, as this can influence the occurrence of mineralizations, namely of W (Mo). To this end, the magnetic mineralogy of the granites of the Lamas de Olo Pluton, a posttectonic pluton in northern Portugal, with associated W (Mo) occurrences was characterized and compared with the magnetic mineralogy of other post-tectonic Variscan plutons. This pluton is composed of different biotite granites: Lamas de Olo, Alto dos Cabeços and Barragem. To better characterize its magnetic behavior, different analytical techniques that complement previous magnetic susceptibility studies were performed. The magnetic mineralogy of Lamas de Olo Pluton was then compared with other post-tectonic Variscan plutons such as the Vila Pouca de Aguiar, Peneda-Gerês and Lavadores-Madalena plutons. The presence of magnetite in some of these granites is important because it points to melt-oxidized conditions not commonly found in Iberian Variscan granites. Our study shows that granite areas where magnetite and/or magnetite/ilmenite coexist are important targets for W (Mo) mineralizations. The results indicate that a few plutons have granites with a complex redox history which leads to the formation of magnetite and ilmenite.
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spelling doaj.art-bf00d46f57fe443981b351eb4d08070a2023-10-20T07:26:33ZengUniversitat de Barcelona (UB), Geociències Barcelona (Geo3BCN), Institut de Diagnosi Ambiental i Estudis de l'Aigua (IDAEA), Universitat Autònoma de Barcelona (UAB)Geologica Acta1696-57282020-03-0118Magnetic mineralogy of Variscan granites from northern Portugal: an approach to their petrogenesis and metallogenic potentialC. Cruz0H. Sant'Ovaia1F. Noronha2Departamento de Geociências Ambiente e Ordenamento do Território - Faculdade de Ciências, Universidade do Porto Rua do Campo Alegre 687, Porto, Portugal.Departamento de Geociências Ambiente e Ordenamento do Território - Faculdade de Ciências, Universidade do Porto Rua do Campo Alegre 687, Porto, Portugal. Instituto de Ciências da Terra, Polo Porto Rua do Campo Alegre 687, Porto, Portugal.Instituto de Ciências da Terra, Polo Porto Rua do Campo Alegre 687, Porto, Portugal Northern Portugal is characterized by the occurrence of numerous W hydrothermal deposits spatially associated with granites. The primary goal of this work is to establish a relationship between the magnetic behavior of the granites and the redox conditions during magma genesis, as this can influence the occurrence of mineralizations, namely of W (Mo). To this end, the magnetic mineralogy of the granites of the Lamas de Olo Pluton, a posttectonic pluton in northern Portugal, with associated W (Mo) occurrences was characterized and compared with the magnetic mineralogy of other post-tectonic Variscan plutons. This pluton is composed of different biotite granites: Lamas de Olo, Alto dos Cabeços and Barragem. To better characterize its magnetic behavior, different analytical techniques that complement previous magnetic susceptibility studies were performed. The magnetic mineralogy of Lamas de Olo Pluton was then compared with other post-tectonic Variscan plutons such as the Vila Pouca de Aguiar, Peneda-Gerês and Lavadores-Madalena plutons. The presence of magnetite in some of these granites is important because it points to melt-oxidized conditions not commonly found in Iberian Variscan granites. Our study shows that granite areas where magnetite and/or magnetite/ilmenite coexist are important targets for W (Mo) mineralizations. The results indicate that a few plutons have granites with a complex redox history which leads to the formation of magnetite and ilmenite. https://revistes.ub.edu/index.php/GEOACTA/article/view/28718Magnetic mineralogyVariscan granitesPost-D3 biotite granitesCentral Iberian ZoneW-Mo mineralizations
spellingShingle C. Cruz
H. Sant'Ovaia
F. Noronha
Magnetic mineralogy of Variscan granites from northern Portugal: an approach to their petrogenesis and metallogenic potential
Geologica Acta
Magnetic mineralogy
Variscan granites
Post-D3 biotite granites
Central Iberian Zone
W-Mo mineralizations
title Magnetic mineralogy of Variscan granites from northern Portugal: an approach to their petrogenesis and metallogenic potential
title_full Magnetic mineralogy of Variscan granites from northern Portugal: an approach to their petrogenesis and metallogenic potential
title_fullStr Magnetic mineralogy of Variscan granites from northern Portugal: an approach to their petrogenesis and metallogenic potential
title_full_unstemmed Magnetic mineralogy of Variscan granites from northern Portugal: an approach to their petrogenesis and metallogenic potential
title_short Magnetic mineralogy of Variscan granites from northern Portugal: an approach to their petrogenesis and metallogenic potential
title_sort magnetic mineralogy of variscan granites from northern portugal an approach to their petrogenesis and metallogenic potential
topic Magnetic mineralogy
Variscan granites
Post-D3 biotite granites
Central Iberian Zone
W-Mo mineralizations
url https://revistes.ub.edu/index.php/GEOACTA/article/view/28718
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AT hsantovaia magneticmineralogyofvariscangranitesfromnorthernportugalanapproachtotheirpetrogenesisandmetallogenicpotential
AT fnoronha magneticmineralogyofvariscangranitesfromnorthernportugalanapproachtotheirpetrogenesisandmetallogenicpotential