Geological reconnaissance of the central part of the Sierra Norte de Córdoba (Continued)

Because of its characteristics, it is a heterogeneous complex of rocks, different from those known of the same age in the other parts of the Sierra de Córdoba and the other southern units of the Sierras Pampeanas system. In the north of our country there have been found quartzite schists little meta...

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Main Author: García Castellanos, Telasco
Format: Online
Language:spa
Published: Universidad Nacional de Córdoba 1943
Subjects:
Online Access:https://revistas.unc.edu.ar/index.php/REUNC/article/view/10543
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author García Castellanos, Telasco
author_facet García Castellanos, Telasco
author_sort García Castellanos, Telasco
collection Portal de Revistas
description Because of its characteristics, it is a heterogeneous complex of rocks, different from those known of the same age in the other parts of the Sierra de Córdoba and the other southern units of the Sierras Pampeanas system. In the north of our country there have been found quartzite schists little metamorphosed that can be identified with the ones we are dealing with.
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spelling oai:ojs.revistas.unc.edu.ar:article-105432023-11-09T18:13:29Z Geological reconnaissance of the central part of the Sierra Norte de Córdoba (Continued) Reconocimiento geológico de la parte central de la Sierra Norte de Córdoba (Continuación) García Castellanos, Telasco Precámbrico Sierras de Córdoba Caminiaga Geología Precambrian Sierras of Córdoba Caminiaga Geology Because of its characteristics, it is a heterogeneous complex of rocks, different from those known of the same age in the other parts of the Sierra de Córdoba and the other southern units of the Sierras Pampeanas system. In the north of our country there have been found quartzite schists little metamorphosed that can be identified with the ones we are dealing with. Por sus características, resulta un complejo heterogéneo de rocas, diferentes a las conocidas de igual edad, en las restantes partes de la Sierra de Córdoba y de las demás unidades australes del sistema de las Sierras Pampeanas. En el Norte de nuestro país se han encontrado esquistos cuarcíticos poco metamorfoseados que se los puede identificar con estos que nos ocupan. Universidad Nacional de Córdoba 1943-07-01 info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion application/pdf https://revistas.unc.edu.ar/index.php/REUNC/article/view/10543 Revista de la Universidad Nacional de Córdoba; Vol. 30 Núm. 5/6 (1943): Julio-Agosto; 571-616 0370-7687 spa https://revistas.unc.edu.ar/index.php/REUNC/article/view/10543/11223 Derechos de autor 1943 Universidad Nacional de Córdoba https://creativecommons.org/licenses/by-nc-sa/4.0
spellingShingle Precámbrico
Sierras de Córdoba
Caminiaga
Geología
Precambrian
Sierras of Córdoba
Caminiaga
Geology
García Castellanos, Telasco
Geological reconnaissance of the central part of the Sierra Norte de Córdoba (Continued)
title Geological reconnaissance of the central part of the Sierra Norte de Córdoba (Continued)
title_alt Reconocimiento geológico de la parte central de la Sierra Norte de Córdoba (Continuación)
title_full Geological reconnaissance of the central part of the Sierra Norte de Córdoba (Continued)
title_fullStr Geological reconnaissance of the central part of the Sierra Norte de Córdoba (Continued)
title_full_unstemmed Geological reconnaissance of the central part of the Sierra Norte de Córdoba (Continued)
title_short Geological reconnaissance of the central part of the Sierra Norte de Córdoba (Continued)
title_sort geological reconnaissance of the central part of the sierra norte de cordoba continued
topic Precámbrico
Sierras de Córdoba
Caminiaga
Geología
Precambrian
Sierras of Córdoba
Caminiaga
Geology
topic_facet Precámbrico
Sierras de Córdoba
Caminiaga
Geología
Precambrian
Sierras of Córdoba
Caminiaga
Geology
url https://revistas.unc.edu.ar/index.php/REUNC/article/view/10543
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