Geochemistry and Geochronology (U-Pb and Lu-Hf) of the Soarinho Alkaline Massif (Brazil): Implications on Mantle versus Crustal Signature of Syenitic Magma

The Soarinho Alkaline Intrusion, southeastern Brazil, makes up part of the Serra do Mar Igneous Province, and it is composed of alkali feldspar syenite, alkali feldspar trachyte, quartz syenite, and monzonite. Geochemical and geochronological analyses of the Soarinho were compared with data from its...

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Main Authors: Daniel Adelino da Silva, Guilherme Loriato Potratz, Mauro Cesar Geraldes
Format: Article
Language:English
Published: MDPI AG 2023-07-01
Series:Minerals
Subjects:
Online Access:https://www.mdpi.com/2075-163X/13/7/904
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author Daniel Adelino da Silva
Guilherme Loriato Potratz
Mauro Cesar Geraldes
author_facet Daniel Adelino da Silva
Guilherme Loriato Potratz
Mauro Cesar Geraldes
author_sort Daniel Adelino da Silva
collection DOAJ
description The Soarinho Alkaline Intrusion, southeastern Brazil, makes up part of the Serra do Mar Igneous Province, and it is composed of alkali feldspar syenite, alkali feldspar trachyte, quartz syenite, and monzonite. Geochemical and geochronological analyses of the Soarinho were compared with data from its neighbors, Rio Bonito and Tanguá. Zircon U-Pb Laser Ablation ages show that Soarinho is younger than Rio Bonito and Tanguá. Ages obtained from the monzonite (60 ± 2 Ma), alkali feldspar syenite (58 ± 2 Ma), and quartz syenite (58 ± 2 Ma) are indistinguishable within error. One nepheline syenite sample from Tanguá gives an age equal to those of Rio Bonito already published (65 ± 1 Ma). Petrographic and geochemical data show a clear contrast among Soarinho, Rio Bonito, and Tanguá. Lu-Hf isotopic data for the three alkaline intrusions (all negative) point to some similarities in their sources. The data suggest an enriched mantle source for Soarinho; however, an older continental crust contribution cannot be discarded.
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spelling doaj.art-c57dd10352294a3c9ce978643345e9ae2023-11-18T20:38:39ZengMDPI AGMinerals2075-163X2023-07-0113790410.3390/min13070904Geochemistry and Geochronology (U-Pb and Lu-Hf) of the Soarinho Alkaline Massif (Brazil): Implications on Mantle versus Crustal Signature of Syenitic MagmaDaniel Adelino da Silva0Guilherme Loriato Potratz1Mauro Cesar Geraldes2Programa de Pós-Graduação em Geociências, Faculdade de Geologia, Universidade do Estado do Rio de Janeiro, Rua São Francisco Xavier, 524, Maracanã, Rio de Janeiro 20950-000, RJ, BrazilPrograma de Pós-Graduação em Geociências, Faculdade de Geologia, Universidade do Estado do Rio de Janeiro, Rua São Francisco Xavier, 524, Maracanã, Rio de Janeiro 20950-000, RJ, BrazilFaculdade de Geologia, Universidade do Estado do Rio de Janeiro, Av. São Francisco Xavier, 524, Sala 2020A, Maracanã, Rio de Janeiro 20950-000, RJ, BrazilThe Soarinho Alkaline Intrusion, southeastern Brazil, makes up part of the Serra do Mar Igneous Province, and it is composed of alkali feldspar syenite, alkali feldspar trachyte, quartz syenite, and monzonite. Geochemical and geochronological analyses of the Soarinho were compared with data from its neighbors, Rio Bonito and Tanguá. Zircon U-Pb Laser Ablation ages show that Soarinho is younger than Rio Bonito and Tanguá. Ages obtained from the monzonite (60 ± 2 Ma), alkali feldspar syenite (58 ± 2 Ma), and quartz syenite (58 ± 2 Ma) are indistinguishable within error. One nepheline syenite sample from Tanguá gives an age equal to those of Rio Bonito already published (65 ± 1 Ma). Petrographic and geochemical data show a clear contrast among Soarinho, Rio Bonito, and Tanguá. Lu-Hf isotopic data for the three alkaline intrusions (all negative) point to some similarities in their sources. The data suggest an enriched mantle source for Soarinho; however, an older continental crust contribution cannot be discarded.https://www.mdpi.com/2075-163X/13/7/904syenitic magma sourcealkali feldspar syenitequartz syeniteU-Pb datingLu-Hf isotopesSoarinho alkaline massif
spellingShingle Daniel Adelino da Silva
Guilherme Loriato Potratz
Mauro Cesar Geraldes
Geochemistry and Geochronology (U-Pb and Lu-Hf) of the Soarinho Alkaline Massif (Brazil): Implications on Mantle versus Crustal Signature of Syenitic Magma
Minerals
syenitic magma source
alkali feldspar syenite
quartz syenite
U-Pb dating
Lu-Hf isotopes
Soarinho alkaline massif
title Geochemistry and Geochronology (U-Pb and Lu-Hf) of the Soarinho Alkaline Massif (Brazil): Implications on Mantle versus Crustal Signature of Syenitic Magma
title_full Geochemistry and Geochronology (U-Pb and Lu-Hf) of the Soarinho Alkaline Massif (Brazil): Implications on Mantle versus Crustal Signature of Syenitic Magma
title_fullStr Geochemistry and Geochronology (U-Pb and Lu-Hf) of the Soarinho Alkaline Massif (Brazil): Implications on Mantle versus Crustal Signature of Syenitic Magma
title_full_unstemmed Geochemistry and Geochronology (U-Pb and Lu-Hf) of the Soarinho Alkaline Massif (Brazil): Implications on Mantle versus Crustal Signature of Syenitic Magma
title_short Geochemistry and Geochronology (U-Pb and Lu-Hf) of the Soarinho Alkaline Massif (Brazil): Implications on Mantle versus Crustal Signature of Syenitic Magma
title_sort geochemistry and geochronology u pb and lu hf of the soarinho alkaline massif brazil implications on mantle versus crustal signature of syenitic magma
topic syenitic magma source
alkali feldspar syenite
quartz syenite
U-Pb dating
Lu-Hf isotopes
Soarinho alkaline massif
url https://www.mdpi.com/2075-163X/13/7/904
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