Geology and petrogenetic considerations of the Loma Marcelo skarn, Neoproterozoic basement of the Ventania System, Argentina

The Late Precambrian–Early Palaeozoic crystalline basement of the Ventania System is mainly composed of Neoproterozoic S-type granites, Early Cambrian alkaline granites, and Middle Cambrian peralkaline rhyolites. The Neoproterozoic granites (<i>ca.</i> 607–581 Ma) crop out in the Cerro P...

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Autores principales: Ballivián Justiniano, Carlos Alberto, Lanfranchini, Mabel Elena, Recio, Clemente, Barrio, Raúl Ernesto de, Sato, Ana María, Basei, Miguel A. S., Pimentel, Marcio M., Etcheverry, Ricardo Oscar, Tassinari, Colombo C. G.
Formato: Articulo
Lenguaje:Inglés
Publicado: 2017
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Acceso en línea:http://sedici.unlp.edu.ar/handle/10915/108963
https://www.sciencedirect.com/science/article/abs/pii/S0301926817302929
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id I19-R120-10915-108963
record_format dspace
institution Universidad Nacional de La Plata
institution_str I-19
repository_str R-120
collection SEDICI (UNLP)
language Inglés
topic Ciencias Naturales
geochemistry
geochronology
carbonate protoliths
polymetamorphism
Sierras Australes of Buenos Aires Province
spellingShingle Ciencias Naturales
geochemistry
geochronology
carbonate protoliths
polymetamorphism
Sierras Australes of Buenos Aires Province
Ballivián Justiniano, Carlos Alberto
Lanfranchini, Mabel Elena
Recio, Clemente
Barrio, Raúl Ernesto de
Sato, Ana María
Basei, Miguel A. S.
Pimentel, Marcio M.
Etcheverry, Ricardo Oscar
Tassinari, Colombo C. G.
Geology and petrogenetic considerations of the Loma Marcelo skarn, Neoproterozoic basement of the Ventania System, Argentina
topic_facet Ciencias Naturales
geochemistry
geochronology
carbonate protoliths
polymetamorphism
Sierras Australes of Buenos Aires Province
description The Late Precambrian–Early Palaeozoic crystalline basement of the Ventania System is mainly composed of Neoproterozoic S-type granites, Early Cambrian alkaline granites, and Middle Cambrian peralkaline rhyolites. The Neoproterozoic granites (<i>ca.</i> 607–581 Ma) crop out in the Cerro Pan de Azúcar-Cerro del Corral area and host the Loma Marcelo Ca/Mg skarn, composed of calc-silicate- and chondrodite-bearing assemblages. Petrographical, geochemical, and geochronological data indicate that the skarn was formed from carbonate xenoliths of sedimentary nature incorporated during the intrusion of the Neoproterozoic granites and that it is the result of three successive metamorphic events. The first one is related to the incorporation of carbonate xenoliths by the intrusion and the associated contact metamorphism. The second event is linked to the crystallization of the Early Cambrian granites and related post-magmatic processes. They are responsible for fluorine influx into the Neoproterozoic basement, which resulted in the formation of high-F minerals in the Loma Marcelo skarn (<i>e.g.</i> vesuvianite, chondrodite). The Sm-Nd garnet-whole rock isochron age of 526.8 ± 12.0 Ma in the skarn confirms its relationship with the Early Cambrian magmatism. The last event corresponds to a regional metamorphism assigned to the Late Devonian–Early Carboniferous on the basis of a LA-ICP-MS U-Pb age of 353.4 ± 6.7 Ma determined on zircons of the skarn as well as a Rb-Sr quartz-sericite isochron age of 364.4 ± 3.6 Ma obtained from a quartz vein that post-tectonically cuts the already mylonitized granites. The different chemical compositions of the carbonate protoliths determined the formation of two types of skarns of calcic and magnesian compositions. A single date of the calcic skarn defined a LA-ICP-MS U-Pb upper intercept age of 648 ± 21 Ma, providing the maximum sedimentation age for the calcic protolith of the Loma Marcelo skarn. The minimum sedimentation age is provided by the crystallization age of the S-type granite surrounding the skarn (<i>ca.</i> 607 Ma). The Loma Marcelo skarn reveals the occurrence of underground Neoproterozoic carbonate (meta-?) sedimentary rocks as part of the basement of the Ventania System. These rocks could correlate with the carbonate sequences of the neighbouring Claromecó Basin and Tandilia System.
format Articulo
Articulo
author Ballivián Justiniano, Carlos Alberto
Lanfranchini, Mabel Elena
Recio, Clemente
Barrio, Raúl Ernesto de
Sato, Ana María
Basei, Miguel A. S.
Pimentel, Marcio M.
Etcheverry, Ricardo Oscar
Tassinari, Colombo C. G.
author_facet Ballivián Justiniano, Carlos Alberto
Lanfranchini, Mabel Elena
Recio, Clemente
Barrio, Raúl Ernesto de
Sato, Ana María
Basei, Miguel A. S.
Pimentel, Marcio M.
Etcheverry, Ricardo Oscar
Tassinari, Colombo C. G.
author_sort Ballivián Justiniano, Carlos Alberto
title Geology and petrogenetic considerations of the Loma Marcelo skarn, Neoproterozoic basement of the Ventania System, Argentina
title_short Geology and petrogenetic considerations of the Loma Marcelo skarn, Neoproterozoic basement of the Ventania System, Argentina
title_full Geology and petrogenetic considerations of the Loma Marcelo skarn, Neoproterozoic basement of the Ventania System, Argentina
title_fullStr Geology and petrogenetic considerations of the Loma Marcelo skarn, Neoproterozoic basement of the Ventania System, Argentina
title_full_unstemmed Geology and petrogenetic considerations of the Loma Marcelo skarn, Neoproterozoic basement of the Ventania System, Argentina
title_sort geology and petrogenetic considerations of the loma marcelo skarn, neoproterozoic basement of the ventania system, argentina
publishDate 2017
url http://sedici.unlp.edu.ar/handle/10915/108963
https://www.sciencedirect.com/science/article/abs/pii/S0301926817302929
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