The fracture patterns of the Tin Tin anticline: Fracturing process during the foreland evolution in the Calchaquí Valley, northwestern Argentina

We present a field-based work which illustrates the fracture patterns of the carbonate-silicoclastic Yacoraite Formation in the Tin Tin anticline, a basement fault-related fold located in southern part of the Eastern Cordillera, northwestern Argentina. The fracture patterns include small-scale strik...

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Autores principales:	Hernández, Mariano, Franzese, Juan Rafael
Formato:	Articulo
Lenguaje:	Inglés
Publicado:	2017
Materias:	Ciencias Naturales Geología Joints Small-scale faults Yacoraite formation Foreland basement-cored fold Eastern Cordillera Northwestern Argentina
Acceso en línea:	http://sedici.unlp.edu.ar/handle/10915/147829
Aporte de:	SEDICI (UNLP) de Universidad Nacional de La Plata

id	I19-R120-10915-147829
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 Geología Joints Small-scale faults Yacoraite formation Foreland basement-cored fold Eastern Cordillera Northwestern Argentina
spellingShingle	Ciencias Naturales Geología Joints Small-scale faults Yacoraite formation Foreland basement-cored fold Eastern Cordillera Northwestern Argentina Hernández, Mariano Franzese, Juan Rafael The fracture patterns of the Tin Tin anticline: Fracturing process during the foreland evolution in the Calchaquí Valley, northwestern Argentina
topic_facet	Ciencias Naturales Geología Joints Small-scale faults Yacoraite formation Foreland basement-cored fold Eastern Cordillera Northwestern Argentina
description	We present a field-based work which illustrates the fracture patterns of the carbonate-silicoclastic Yacoraite Formation in the Tin Tin anticline, a basement fault-related fold located in southern part of the Eastern Cordillera, northwestern Argentina. The fracture patterns include small-scale strike-slip faults (vertical shear fractures and en echelon arrays), thrust faults, extension fractures (joints, veins and normal faults) and stylolites. Extensional mesostructures were formed by along-foreland stretching, prior to the contractional ones that were formed by the layer-parallel shortening mechanism. Furthermore, all fractures are interpreted to be formed before or at the early stages of folding and thrusting during the Andean contraction, all of them belonging to the Eocene thrust belt-foreland system at the Calchaquí Valley of northwestern Argentina.
format	Articulo Articulo
author	Hernández, Mariano Franzese, Juan Rafael
author_facet	Hernández, Mariano Franzese, Juan Rafael
author_sort	Hernández, Mariano
title	The fracture patterns of the Tin Tin anticline: Fracturing process during the foreland evolution in the Calchaquí Valley, northwestern Argentina
title_short	The fracture patterns of the Tin Tin anticline: Fracturing process during the foreland evolution in the Calchaquí Valley, northwestern Argentina
title_full	The fracture patterns of the Tin Tin anticline: Fracturing process during the foreland evolution in the Calchaquí Valley, northwestern Argentina
title_fullStr	The fracture patterns of the Tin Tin anticline: Fracturing process during the foreland evolution in the Calchaquí Valley, northwestern Argentina
title_full_unstemmed	The fracture patterns of the Tin Tin anticline: Fracturing process during the foreland evolution in the Calchaquí Valley, northwestern Argentina
title_sort	fracture patterns of the tin tin anticline: fracturing process during the foreland evolution in the calchaquí valley, northwestern argentina
publishDate	2017
url	http://sedici.unlp.edu.ar/handle/10915/147829
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The fracture patterns of the Tin Tin anticline: Fracturing process during the foreland evolution in the Calchaquí Valley, northwestern Argentina

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