Metallogenic evolution of the Sierras Pampeanas of Córdoba and south of Santiago del Estero: Famatinian, Gondwanic and Andean cycles

Five metallogenic stages are proposed for the metallogenic evolution of the Sierra Pampeaneas of Córdoba and south of Santiago del Estero, havin. having already been exposed the first two previous work. Metallogenic stage 3, corresponding to the second orogenic cycle of the Pampean-Famatinian compre...

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Publicado: 2005
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Acceso en línea:https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_00044822_v60_n3_p467_Mutti
http://hdl.handle.net/20.500.12110/paper_00044822_v60_n3_p467_Mutti
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spelling paper:paper_00044822_v60_n3_p467_Mutti2023-06-08T14:25:55Z Metallogenic evolution of the Sierras Pampeanas of Córdoba and south of Santiago del Estero: Famatinian, Gondwanic and Andean cycles Andean Córdoba Famatinian Gondwanic Metallogenesis Mineralized belts Ore deposit Santiago del Estero Sierras Pampeanas Gondwana metallogenesis mineralization ore deposit orogenic belt tectonic evolution Argentina Sierras Pampeanas South America Five metallogenic stages are proposed for the metallogenic evolution of the Sierra Pampeaneas of Córdoba and south of Santiago del Estero, havin. having already been exposed the first two previous work. Metallogenic stage 3, corresponding to the second orogenic cycle of the Pampean-Famatinian compressive cycle, was characterized by hydrothermal fluid migration and the generation and reactivation of the main structures. At the same time, transformations occurred in deposits of Cr (Fe-Ti), Cu (Au-Ag), Pb-Zn (Ag-Cu-Au), Fe and Cu-Fe (Zn-Au-Ag-Co), and Be-Nb-Ta-W-P-U-ETR -rich pegmatites originated, together with biextended deposits of W-Bi (Mo-Cu-Sn-Zn-Au-B-F-Te), of U in association with granitoids, metasomatic deposits of Fe-Cu (Ti-Au), and Au (Cu-Zn-Pb-As) rich veins and Ag-Pb-Zn (V-Sn-Mn-Cd-Au-Cu-As-Bi-Sb-Co) rich veins. These deposits are correlated with those of orogenic belts. In the course of metallogenic stage 4, corresponding to the Gondwanic extensional cycle and related to the early opening of the Atlantic rift, Mn (Fe-F-Ba) -rich veins, and F (Fe-Mn) -rich veins were formed in association with granitoids. Metallogenic stage 5 developed during the Andean compressive cycle, generating epithermal Au occurrences, and deposits and occurrences of U-V (Mn-Fe) in sedimentary rocks. The successive stages of deposition and mobilization of metallic elements determined mineralized belts in this part of Sierras Pampeanas giving birth to a specialized domain in Cr, W, Fe, Cu, Zn, Pb, Ti, Au, Bi, Be, Li, U, Mn, F and B, with Sn, Mo, ETR, Ta, Nb, V, Cd, Ag, Sb, Co, P, As, S, Te, Se and Ba subordinated. © 2005 Asociación Geológica Argentina. 2005 https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_00044822_v60_n3_p467_Mutti http://hdl.handle.net/20.500.12110/paper_00044822_v60_n3_p467_Mutti
institution Universidad de Buenos Aires
institution_str I-28
repository_str R-134
collection Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA)
topic Andean
Córdoba
Famatinian
Gondwanic
Metallogenesis
Mineralized belts
Ore deposit
Santiago del Estero
Sierras Pampeanas
Gondwana
metallogenesis
mineralization
ore deposit
orogenic belt
tectonic evolution
Argentina
Sierras Pampeanas
South America
spellingShingle Andean
Córdoba
Famatinian
Gondwanic
Metallogenesis
Mineralized belts
Ore deposit
Santiago del Estero
Sierras Pampeanas
Gondwana
metallogenesis
mineralization
ore deposit
orogenic belt
tectonic evolution
Argentina
Sierras Pampeanas
South America
Metallogenic evolution of the Sierras Pampeanas of Córdoba and south of Santiago del Estero: Famatinian, Gondwanic and Andean cycles
topic_facet Andean
Córdoba
Famatinian
Gondwanic
Metallogenesis
Mineralized belts
Ore deposit
Santiago del Estero
Sierras Pampeanas
Gondwana
metallogenesis
mineralization
ore deposit
orogenic belt
tectonic evolution
Argentina
Sierras Pampeanas
South America
description Five metallogenic stages are proposed for the metallogenic evolution of the Sierra Pampeaneas of Córdoba and south of Santiago del Estero, havin. having already been exposed the first two previous work. Metallogenic stage 3, corresponding to the second orogenic cycle of the Pampean-Famatinian compressive cycle, was characterized by hydrothermal fluid migration and the generation and reactivation of the main structures. At the same time, transformations occurred in deposits of Cr (Fe-Ti), Cu (Au-Ag), Pb-Zn (Ag-Cu-Au), Fe and Cu-Fe (Zn-Au-Ag-Co), and Be-Nb-Ta-W-P-U-ETR -rich pegmatites originated, together with biextended deposits of W-Bi (Mo-Cu-Sn-Zn-Au-B-F-Te), of U in association with granitoids, metasomatic deposits of Fe-Cu (Ti-Au), and Au (Cu-Zn-Pb-As) rich veins and Ag-Pb-Zn (V-Sn-Mn-Cd-Au-Cu-As-Bi-Sb-Co) rich veins. These deposits are correlated with those of orogenic belts. In the course of metallogenic stage 4, corresponding to the Gondwanic extensional cycle and related to the early opening of the Atlantic rift, Mn (Fe-F-Ba) -rich veins, and F (Fe-Mn) -rich veins were formed in association with granitoids. Metallogenic stage 5 developed during the Andean compressive cycle, generating epithermal Au occurrences, and deposits and occurrences of U-V (Mn-Fe) in sedimentary rocks. The successive stages of deposition and mobilization of metallic elements determined mineralized belts in this part of Sierras Pampeanas giving birth to a specialized domain in Cr, W, Fe, Cu, Zn, Pb, Ti, Au, Bi, Be, Li, U, Mn, F and B, with Sn, Mo, ETR, Ta, Nb, V, Cd, Ag, Sb, Co, P, As, S, Te, Se and Ba subordinated. © 2005 Asociación Geológica Argentina.
title Metallogenic evolution of the Sierras Pampeanas of Córdoba and south of Santiago del Estero: Famatinian, Gondwanic and Andean cycles
title_short Metallogenic evolution of the Sierras Pampeanas of Córdoba and south of Santiago del Estero: Famatinian, Gondwanic and Andean cycles
title_full Metallogenic evolution of the Sierras Pampeanas of Córdoba and south of Santiago del Estero: Famatinian, Gondwanic and Andean cycles
title_fullStr Metallogenic evolution of the Sierras Pampeanas of Córdoba and south of Santiago del Estero: Famatinian, Gondwanic and Andean cycles
title_full_unstemmed Metallogenic evolution of the Sierras Pampeanas of Córdoba and south of Santiago del Estero: Famatinian, Gondwanic and Andean cycles
title_sort metallogenic evolution of the sierras pampeanas of córdoba and south of santiago del estero: famatinian, gondwanic and andean cycles
publishDate 2005
url https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_00044822_v60_n3_p467_Mutti
http://hdl.handle.net/20.500.12110/paper_00044822_v60_n3_p467_Mutti
_version_ 1768545764751966208