Subvolcanic petrology of the Pico dos Três Estados region (SE Brazil): Implications for Alkaline Magmatic Evolution

Abstract This paper presents a geological study of the subvolcanic bodies present in the Pico dos Três Estados (São Paulo (SP), Rio de Janeiro (RJ), and Minas Gerais (MG)) and its surroundings at the Passa Quatro Alkaline Complex. In this study, we used field-collected data, petrography, and geochem...

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Main Authors: Graciano Carlos de Freitas, Artur Corval, Júlio Cesar Lopes da Silva, Helena Saraiva Koenow Pinheiro, Sérgio de Castro Valente
Format: Article
Language:English
Published: Sociedade Brasileira de Geologia 2025-02-01
Series:Brazilian Journal of Geology
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Online Access:http://www.scielo.br/scielo.php?script=sci_arttext&pid=S2317-48892025000100300&lng=en&tlng=en
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author Graciano Carlos de Freitas
Artur Corval
Júlio Cesar Lopes da Silva
Helena Saraiva Koenow Pinheiro
Sérgio de Castro Valente
author_facet Graciano Carlos de Freitas
Artur Corval
Júlio Cesar Lopes da Silva
Helena Saraiva Koenow Pinheiro
Sérgio de Castro Valente
author_sort Graciano Carlos de Freitas
collection DOAJ
description Abstract This paper presents a geological study of the subvolcanic bodies present in the Pico dos Três Estados (São Paulo (SP), Rio de Janeiro (RJ), and Minas Gerais (MG)) and its surroundings at the Passa Quatro Alkaline Complex. In this study, we used field-collected data, petrography, and geochemical analysis data. From a more detailed fieldwork, we verified that the region that appeared to present only two lithologies in previous works presented a faciological complex with at least six distinct facies, with emphasis on the phonolitic body that forms the Pico dos Três Estados (2,665 m high). Still regarding fieldwork, we found that there are signs of magma mingling processes in the area. Modeling indicates that 10% of fractional crystallization was able to derive the phonolitic rocks from a trachytic liquid based on the following elements: Y, Nb, Yb, Ce, Sm, Eu, La, Nd, Hf, and Pr. The modal batch partial melting shows the possible mantle sources for the magmatism in this area. This data pointed out the involvement of an enriched mantle source in the La/Yb ratio by at least 16 times more than an Oceanic Island Basalt (OIB)-type mantle.
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issn 2317-4692
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series Brazilian Journal of Geology
spelling doaj-art-74f177ba83fa4071abef43248a56f9022025-02-04T07:40:07ZengSociedade Brasileira de GeologiaBrazilian Journal of Geology2317-46922025-02-015510.1590/2317-4889202520240009Subvolcanic petrology of the Pico dos Três Estados region (SE Brazil): Implications for Alkaline Magmatic EvolutionGraciano Carlos de Freitashttps://orcid.org/0000-0001-5796-7632Artur Corvalhttps://orcid.org/0000-0002-5154-2737Júlio Cesar Lopes da Silvahttps://orcid.org/0000-0001-6230-0058Helena Saraiva Koenow Pinheirohttps://orcid.org/0000-0001-5742-7556Sérgio de Castro Valentehttps://orcid.org/0000-0002-7467-672XAbstract This paper presents a geological study of the subvolcanic bodies present in the Pico dos Três Estados (São Paulo (SP), Rio de Janeiro (RJ), and Minas Gerais (MG)) and its surroundings at the Passa Quatro Alkaline Complex. In this study, we used field-collected data, petrography, and geochemical analysis data. From a more detailed fieldwork, we verified that the region that appeared to present only two lithologies in previous works presented a faciological complex with at least six distinct facies, with emphasis on the phonolitic body that forms the Pico dos Três Estados (2,665 m high). Still regarding fieldwork, we found that there are signs of magma mingling processes in the area. Modeling indicates that 10% of fractional crystallization was able to derive the phonolitic rocks from a trachytic liquid based on the following elements: Y, Nb, Yb, Ce, Sm, Eu, La, Nd, Hf, and Pr. The modal batch partial melting shows the possible mantle sources for the magmatism in this area. This data pointed out the involvement of an enriched mantle source in the La/Yb ratio by at least 16 times more than an Oceanic Island Basalt (OIB)-type mantle.http://www.scielo.br/scielo.php?script=sci_arttext&pid=S2317-48892025000100300&lng=en&tlng=enfractional crystallizationpartial meltingmagma minglingsubvolcanic rocks
spellingShingle Graciano Carlos de Freitas
Artur Corval
Júlio Cesar Lopes da Silva
Helena Saraiva Koenow Pinheiro
Sérgio de Castro Valente
Subvolcanic petrology of the Pico dos Três Estados region (SE Brazil): Implications for Alkaline Magmatic Evolution
Brazilian Journal of Geology
fractional crystallization
partial melting
magma mingling
subvolcanic rocks
title Subvolcanic petrology of the Pico dos Três Estados region (SE Brazil): Implications for Alkaline Magmatic Evolution
title_full Subvolcanic petrology of the Pico dos Três Estados region (SE Brazil): Implications for Alkaline Magmatic Evolution
title_fullStr Subvolcanic petrology of the Pico dos Três Estados region (SE Brazil): Implications for Alkaline Magmatic Evolution
title_full_unstemmed Subvolcanic petrology of the Pico dos Três Estados region (SE Brazil): Implications for Alkaline Magmatic Evolution
title_short Subvolcanic petrology of the Pico dos Três Estados region (SE Brazil): Implications for Alkaline Magmatic Evolution
title_sort subvolcanic petrology of the pico dos tres estados region se brazil implications for alkaline magmatic evolution
topic fractional crystallization
partial melting
magma mingling
subvolcanic rocks
url http://www.scielo.br/scielo.php?script=sci_arttext&pid=S2317-48892025000100300&lng=en&tlng=en
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