Horizontal stress Field evolution from Eocene to present in Neuquen Basin

Continuity and evolution in time of the horizontal stress direction in the Neuquen Basin area, derived from the analysis of recent borehole data and orientation of volcanic dykes measured in outcrop in the Cara Cura and Reyes Ranges is presented. The bitumen dykes along the Neuquén Basin were formed...

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Detalles Bibliográficos
Autores principales:	Guzmán, Cecilia Griselda, Cristallini, Ernesto Osvaldo, García, Víctor Hugo, Yagupsky, Daniel Leonardo, Bechis, Florencia
Publicado:	2011
Materias:	Breakout Central andes Dikes Retroarc Stress basin evolution bitumen borehole dike Eocene Paleocene stress field structural geology uncertainty analysis Argentina Neuquen Basin Cura
Acceso en línea:	https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_00044822_v68_n4_p542_Guzman http://hdl.handle.net/20.500.12110/paper_00044822_v68_n4_p542_Guzman
Aporte de:	Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA) de Universidad de Buenos Aires

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