Marine Phosphates in the Paleogene oflsla Grande de Tîerra del Fuego

Phosphate prospecting in marine sedimentary rocks of the Marginal and Austral basins of the Isla Grande de Tierra del Fuego resulted in the first discovery of phosphatic beds in the Paleogene Rio Claro Formation. Phosphatic anomalies of up to 20.1% P2U5 in concretions and up to 2% PaOs in bulk rock...

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Autores principales: Olivero, E.B., Castrq, L.N., Scasso, R.A., Faziq, A.M., Miretzky, P.
Formato: Artículo publishedVersion
Publicado: 1998
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Acceso en línea:http://hdl.handle.net/20.500.12110/paper_00044822_v53_n2_p239_Olivero
https://repositoriouba.sisbi.uba.ar/gsdl/cgi-bin/library.cgi?a=d&c=artiaex&d=paper_00044822_v53_n2_p239_Olivero_oai
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id I28-R145-paper_00044822_v53_n2_p239_Olivero_oai
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spelling I28-R145-paper_00044822_v53_n2_p239_Olivero_oai2024-08-16 Olivero, E.B. Castrq, L.N. Scasso, R.A. Faziq, A.M. Miretzky, P. 1998 Phosphate prospecting in marine sedimentary rocks of the Marginal and Austral basins of the Isla Grande de Tierra del Fuego resulted in the first discovery of phosphatic beds in the Paleogene Rio Claro Formation. Phosphatic anomalies of up to 20.1% P2U5 in concretions and up to 2% PaOs in bulk rock offer promising opportunities for systematic prospection on the Isla Grande de Tierra del Fuego. The phosphatic beds are conglomerates, coquinas and conglomeratic sandstones interbedded with thick mudstone packets. They belong to the condensed-type phosphatic beds, which are the product of erosion and reworking of concretions developed in fine sediments. Phosphate concretions containing glauconite, together with abundant glauconite in the same and closely associated beds, indicate a common syn-sedimentary to earlydiagenetic origin for both minerals, via recycling of sedimentary iron. This process occurred on a shelf with low sedimentation rates, pointing to high sea-level stands and marked interruptions in the sedimentation of the thick Paleogene sedimentary sequence of the Austral Basin . The deposit point to the existence and extension of this early Cenozoic phosphogenic episode to high latitudes in the Southern Hemisphere. © 1998 Asociacidn Geoldgica Argentina. Fil:Olivero, E.B. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. Fil:Scasso, R.A. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. Fil:Miretzky, P. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. application/pdf http://hdl.handle.net/20.500.12110/paper_00044822_v53_n2_p239_Olivero info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by/2.5/ar Rev. Asoc. Geol. Argent. 1998;53(2):239-246 marine sediment Paleogene phosphate South America Marine Phosphates in the Paleogene oflsla Grande de Tîerra del Fuego info:eu-repo/semantics/article info:ar-repo/semantics/artículo info:eu-repo/semantics/publishedVersion https://repositoriouba.sisbi.uba.ar/gsdl/cgi-bin/library.cgi?a=d&c=artiaex&d=paper_00044822_v53_n2_p239_Olivero_oai
institution Universidad de Buenos Aires
institution_str I-28
repository_str R-145
collection Repositorio Digital de la Universidad de Buenos Aires (UBA)
topic marine sediment
Paleogene
phosphate
South America
spellingShingle marine sediment
Paleogene
phosphate
South America
Olivero, E.B.
Castrq, L.N.
Scasso, R.A.
Faziq, A.M.
Miretzky, P.
Marine Phosphates in the Paleogene oflsla Grande de Tîerra del Fuego
topic_facet marine sediment
Paleogene
phosphate
South America
description Phosphate prospecting in marine sedimentary rocks of the Marginal and Austral basins of the Isla Grande de Tierra del Fuego resulted in the first discovery of phosphatic beds in the Paleogene Rio Claro Formation. Phosphatic anomalies of up to 20.1% P2U5 in concretions and up to 2% PaOs in bulk rock offer promising opportunities for systematic prospection on the Isla Grande de Tierra del Fuego. The phosphatic beds are conglomerates, coquinas and conglomeratic sandstones interbedded with thick mudstone packets. They belong to the condensed-type phosphatic beds, which are the product of erosion and reworking of concretions developed in fine sediments. Phosphate concretions containing glauconite, together with abundant glauconite in the same and closely associated beds, indicate a common syn-sedimentary to earlydiagenetic origin for both minerals, via recycling of sedimentary iron. This process occurred on a shelf with low sedimentation rates, pointing to high sea-level stands and marked interruptions in the sedimentation of the thick Paleogene sedimentary sequence of the Austral Basin . The deposit point to the existence and extension of this early Cenozoic phosphogenic episode to high latitudes in the Southern Hemisphere. © 1998 Asociacidn Geoldgica Argentina.
format Artículo
Artículo
publishedVersion
author Olivero, E.B.
Castrq, L.N.
Scasso, R.A.
Faziq, A.M.
Miretzky, P.
author_facet Olivero, E.B.
Castrq, L.N.
Scasso, R.A.
Faziq, A.M.
Miretzky, P.
author_sort Olivero, E.B.
title Marine Phosphates in the Paleogene oflsla Grande de Tîerra del Fuego
title_short Marine Phosphates in the Paleogene oflsla Grande de Tîerra del Fuego
title_full Marine Phosphates in the Paleogene oflsla Grande de Tîerra del Fuego
title_fullStr Marine Phosphates in the Paleogene oflsla Grande de Tîerra del Fuego
title_full_unstemmed Marine Phosphates in the Paleogene oflsla Grande de Tîerra del Fuego
title_sort marine phosphates in the paleogene oflsla grande de tîerra del fuego
publishDate 1998
url http://hdl.handle.net/20.500.12110/paper_00044822_v53_n2_p239_Olivero
https://repositoriouba.sisbi.uba.ar/gsdl/cgi-bin/library.cgi?a=d&c=artiaex&d=paper_00044822_v53_n2_p239_Olivero_oai
work_keys_str_mv AT oliveroeb marinephosphatesinthepaleogeneoflslagrandedetierradelfuego
AT castrqln marinephosphatesinthepaleogeneoflslagrandedetierradelfuego
AT scassora marinephosphatesinthepaleogeneoflslagrandedetierradelfuego
AT faziqam marinephosphatesinthepaleogeneoflslagrandedetierradelfuego
AT miretzkyp marinephosphatesinthepaleogeneoflslagrandedetierradelfuego
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