Termobarometría núcleo-borde en granates con zonado difusíonal: El ejemplo del Domo Gneísico del Tormes, NO de Salamanca
| dc.contributor.author | Escuder Viruete, Javier | |
| dc.contributor.author | Indares, A. | |
| dc.contributor.author | Arenas, R. | |
| dc.date.accessioned | 2016-06-22T08:40:47Z | |
| dc.date.available | 2016-06-22T08:40:47Z | |
| dc.date.issued | 1996 | |
| dc.description.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 | en_US |
| dc.identifier.uri | http://hdl.handle.net/10272/12407 | |
| dc.language.iso | spa | en_US |
| dc.publisher | Sociedad Geológica de España | en_US |
| dc.rights | Atribución-NoComercial-SinDerivadas 3.0 España | * |
| dc.rights.accessRights | open access | en_US |
| dc.rights.uri | http://creativecommons.org/licenses/by-nc-nd/3.0/es/ | * |
| dc.subject.other | Diffusional zoned garnets | en_US |
| dc.subject.other | Core-rim thermobarometry | en_US |
| dc.subject.other | P-T path | en_US |
| dc.subject.other | Tormes Gneissic Dome | en_US |
| dc.subject.other | Iberian Massif | en_US |
| dc.title | Termobarometría núcleo-borde en granates con zonado difusíonal: El ejemplo del Domo Gneísico del Tormes, NO de Salamanca | en_US |
| dc.title | Core-Rim thermobarometry in cliffusional zoned garnets: An example from the Tormes Gneissic Dome, NW Salamanca | eng |
| dc.type | journal article | en_US |
| dspace.entity.type | Publication |
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