Geology of the Quebrada Honda, basin of Lago La Plata, Chubut

The quebrada Honda is situated in the Lago La Plata-Fontana basin in Chubut. The stratigraphy of the area begins in the Upper Jurassic with the calc-alkaline intermediate to acidic Lago La Plata Formation rocks. The Neocomian Coyhaique Group, which includes the Tres Lagunas and Katterfeld Formations...

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Detalles Bibliográficos
Autores principales:	Depine, G.V., Ramos, V.A.
Formato:	JOUR
Materias:	Intraarc Lago La Plata Neocomian Quebrada Honda Tectonic inversion basin fill sedimentary rock stratigraphy systems tract tectonic setting transgression volcanic rock La Plata Basin South America Western Hemisphere World
Acceso en línea:	http://hdl.handle.net/20.500.12110/paper_00044822_v59_n4_p643_Depine
Aporte de:	Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA) de Universidad de Buenos Aires

id	todo:paper_00044822_v59_n4_p643_Depine
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spelling	todo:paper_00044822_v59_n4_p643_Depine2023-10-03T13:58:00Z Geology of the Quebrada Honda, basin of Lago La Plata, Chubut Depine, G.V. Ramos, V.A. Intraarc Lago La Plata Neocomian Quebrada Honda Tectonic inversion basin fill sedimentary rock stratigraphy systems tract tectonic setting transgression volcanic rock La Plata Basin South America Western Hemisphere World The quebrada Honda is situated in the Lago La Plata-Fontana basin in Chubut. The stratigraphy of the area begins in the Upper Jurassic with the calc-alkaline intermediate to acidic Lago La Plata Formation rocks. The Neocomian Coyhaique Group, which includes the Tres Lagunas and Katterfeld Formations, is the sedimentary filling of the intraarc basin that was developed by that time. These units are included in a paleoenviromental model as a shelf-margin system tract followed by a transgressive system tract. The discovery of Favrella americana in the Katterfeld Formation constrains to the Early Hauterivian the age of these sequences. The hypabissal calc-alkaline Quebrada Honda Gabbro is related to extension as well as the more evolved Late Neocomian Don Rueda Formation volcanism. This subaerial magmatic event shows evidences of interaction with aqueous bodies that indicate the concomitance with the last sedimentary Coyhaique Group filling of the basin. A maximum age of 80 My is assigned to the tectonic inversion observed in the area. © 2004 Asociación Geológica Argentina. JOUR info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by/2.5/ar http://hdl.handle.net/20.500.12110/paper_00044822_v59_n4_p643_Depine
institution	Universidad de Buenos Aires
institution_str	I-28
repository_str	R-134
collection	Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA)
topic	Intraarc Lago La Plata Neocomian Quebrada Honda Tectonic inversion basin fill sedimentary rock stratigraphy systems tract tectonic setting transgression volcanic rock La Plata Basin South America Western Hemisphere World
spellingShingle	Intraarc Lago La Plata Neocomian Quebrada Honda Tectonic inversion basin fill sedimentary rock stratigraphy systems tract tectonic setting transgression volcanic rock La Plata Basin South America Western Hemisphere World Depine, G.V. Ramos, V.A. Geology of the Quebrada Honda, basin of Lago La Plata, Chubut
topic_facet	Intraarc Lago La Plata Neocomian Quebrada Honda Tectonic inversion basin fill sedimentary rock stratigraphy systems tract tectonic setting transgression volcanic rock La Plata Basin South America Western Hemisphere World
description	The quebrada Honda is situated in the Lago La Plata-Fontana basin in Chubut. The stratigraphy of the area begins in the Upper Jurassic with the calc-alkaline intermediate to acidic Lago La Plata Formation rocks. The Neocomian Coyhaique Group, which includes the Tres Lagunas and Katterfeld Formations, is the sedimentary filling of the intraarc basin that was developed by that time. These units are included in a paleoenviromental model as a shelf-margin system tract followed by a transgressive system tract. The discovery of Favrella americana in the Katterfeld Formation constrains to the Early Hauterivian the age of these sequences. The hypabissal calc-alkaline Quebrada Honda Gabbro is related to extension as well as the more evolved Late Neocomian Don Rueda Formation volcanism. This subaerial magmatic event shows evidences of interaction with aqueous bodies that indicate the concomitance with the last sedimentary Coyhaique Group filling of the basin. A maximum age of 80 My is assigned to the tectonic inversion observed in the area. © 2004 Asociación Geológica Argentina.
format	JOUR
author	Depine, G.V. Ramos, V.A.
author_facet	Depine, G.V. Ramos, V.A.
author_sort	Depine, G.V.
title	Geology of the Quebrada Honda, basin of Lago La Plata, Chubut
title_short	Geology of the Quebrada Honda, basin of Lago La Plata, Chubut
title_full	Geology of the Quebrada Honda, basin of Lago La Plata, Chubut
title_fullStr	Geology of the Quebrada Honda, basin of Lago La Plata, Chubut
title_full_unstemmed	Geology of the Quebrada Honda, basin of Lago La Plata, Chubut
title_sort	geology of the quebrada honda, basin of lago la plata, chubut
url	http://hdl.handle.net/20.500.12110/paper_00044822_v59_n4_p643_Depine
work_keys_str_mv	AT depinegv geologyofthequebradahondabasinoflagolaplatachubut AT ramosva geologyofthequebradahondabasinoflagolaplatachubut
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Geology of the Quebrada Honda, basin of Lago La Plata, Chubut

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