RT Journal Article
T1 Termobarometría núcleo-borde en granates con zonado difusíonal: El ejemplo del Domo Gneísico del Tormes, NO de Salamanca
T1 Core-Rim thermobarometry in cliffusional zoned garnets: An example from the Tormes Gneissic Dome, NW Salamanca
A1 Escuder Viruete, Javier
A1 Indares, A.
A1 Arenas, R.
AB 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
PB Sociedad Geológica de España
YR 1996
FD 1996
LK http://hdl.handle.net/10272/12407
UL http://hdl.handle.net/10272/12407
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 30 may 2026