The "Ñireco Caldera" in the central-western Neuquén Andes (38°50'S - 70°50'O)
In the southern segment of the Copahue- Pino Hachado block, next to the Moquehue-Alumine lacustrine basin, an anomalous concentration of calderas, resulting from a Pliocene-Quaternary volcanic activity was recognized. The Ñireco caldera, which was proposed as part of this caldera complex, is the rea...
Autor principal: | Garcia Morabito, Ezequiel |
---|---|
Publicado: |
2010
|
Materias: | |
Acceso en línea: | https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_00044822_v67_n2_p177_GonzalezDiaz http://hdl.handle.net/20.500.12110/paper_00044822_v67_n2_p177_GonzalezDiaz |
Aporte de: |
Ejemplares similares
-
The "Ñireco Caldera" in the central-western Neuquén Andes (38°50'S - 70°50'O)
por: González Díaz, E.F., et al.
Publicado: (2010) -
The "Ñireco Caldera" in the central-western Neuquén Andes (38°50'S - 70°50'O)
por: González Díaz, E.F., et al. -
The "Ñireco Caldera" in the central-western Neuquén Andes (38°50'S - 70°50'O)
por: González Díaz, E.F., et al.
Publicado: (2010) -
The Copahue-Pino Hachado high and the Loncopuè trough: An episodic tectonic behaviour, Neuquén Andes (37°-39°S)
por: Morabito, E.G., et al.
Publicado: (2005) -
The Copahue-Pino Hachado high and the Loncopuè trough: An episodic tectonic behaviour, Neuquén Andes (37°-39°S)
por: Morabito, E.G., et al.