@article{10272/12407,
year = {1996},
url = {http://hdl.handle.net/10272/12407},
abstract = {Metapelites and add orthogneisses from the Lower Unit of the Tormes Gneissic Dome, NW Salamanca, contain high-grade mineral assemblages with characteristics diffusional zoned garnets, The P-T path deduced for this unit from combined studies based on TWEEQU thermobarometry in core-rim garnets, retrograde reaction analysis and mineral zoning, shows an important isothermal decompression of several kilobars. This decompression is the record of the tectonic exhumation of the unit, caused by a D2 extenslonal event related with the collapse of the previously thickened Variscan crust},
publisher = {Sociedad Geológica de España},
keywords = {Diffusional zoned garnets},
keywords = {Core-rim thermobarometry},
keywords = {P-T path},
keywords = {Tormes Gneissic Dome},
keywords = {Iberian Massif},
title = {Termobarometría núcleo-borde en granates con zonado difusíonal: El ejemplo del Domo Gneísico del Tormes, NO de Salamanca},
title = {Core-Rim thermobarometry in cliffusional zoned garnets: An example from the Tormes Gneissic Dome, NW Salamanca},
author = {Escuder Viruete, J. and Indares, A. and Arenas, R.},
}