CADIC 02618
CENTRO AUSTRAL DE INVESTIGACIONES CIENTIFICAS
Unidad Ejecutora - UE
congresos y reuniones científicas
Título:
The monte Kranck pluton: a new evidence of magmatic activity in the Fuegian Andes of Argentina
Autor/es:
GONZÁLEZ GUILLOT, M.; ACEVEDO, R.; ESCAYOLA, M.
Lugar:
Santiago de Chile
Reunión:
Congreso; GeoSur 2007; 2007
Institución organizadora:
Pontificia Universidad Católica de Chile
Resumen:
A plutonic body recently discovered immediately to the south of these mafic dikes could be petrographically correlated with Jeu Jepen Diorite, both emplaced in Beauvoir Formation, to the east. These intrusions are separated by 65 km through a displacement of sinestral transcurrent fault. The first one belongs, tectonically speaking, to the South America Plate and the second, to the Scotia Plate. Astonishingly identical geological setting in spite of different tectonic plates.
