INGEIS   05370
INSTITUTO DE GEOCRONOLOGIA Y GEOLOGIA ISOTOPICA
Unidad Ejecutora - UE
congresos y reuniones científicas
Título:
Electrical conductivity beneath the Andean back-arc in Argentina near 36.5 S
Autor/es:
A. BURD, J. BOOKER, A. FAVETTO, M. C. POMPOSIELLO, G.GIORDANENGO.
Lugar:
El Vendrell España
Reunión:
Workshop; 18th International Workshop on Electromagnetic Induction in the Earth; 2006
Resumen:
S. Mendoza Province, south of the Nazca flat slab, has widespread recent
basaltic volcanism, but no historic activity. Over the last 1 MY, the basalt has
evolved from having a slab signature to OIB. In early 2005, we collected 18 MT
sites from 67 to 70 W along 36.7 S, near the large caldera Pay´un Matr´u. For a
subset of these significantly 3D data, we can justify a regional strike determined
from phase tensors and induction vectors of about N 19 W at periods below
200 s and N 33 W at longer periods. Minimum structure 2D inversions of
both period ranges imply resistive crust except near the surface. There is no
high conductivity clearly causally related to the basaltic volcanism. At the
west end of our profile there is lower crustal to upper mantle conductivity that
decreases and deepens eastward, which seems more likely to be related to the
active Andean volcanic arc.