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Core-Rim thermobarometry in cliffusional zoned garnets: An example from the Tormes Gneissic Dome, NW Salamanca

dc.contributor.authorEscuder Viruete, J.
dc.contributor.authorIndares, A.
dc.contributor.authorArenas, R.
dc.description.abstractMetapelites 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 crusten_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.subject.otherDiffusional zoned garnetsen_US
dc.subject.otherCore-rim thermobarometryen_US
dc.subject.otherP-T pathen_US
dc.subject.otherTormes Gneissic Domeen_US
dc.subject.otherIberian Massifen_US
dc.titleTermobarometría núcleo-borde en granates con zonado difusíonal: El ejemplo del Domo Gneísico del Tormes, NO de Salamancaen_US
dc.titleCore-Rim thermobarometry in cliffusional zoned garnets: An example from the Tormes Gneissic Dome, NW Salamancaeng

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Atribución-NoComercial-SinDerivadas 3.0 España
Except where otherwise noted, this item's license is described as Atribución-NoComercial-SinDerivadas 3.0 España

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