Nueva interpretación petrológica y tectónica de las anfibolitas pobres en calcio del antiforme de Arinteiro (NO del Macizo Ibérico). II: Estructura e implicaciones para la génesis de anfibolitas pobres en calcio

dc.contributor.authorGómez Barreiro, Juan
dc.contributor.authorCastiñeiras, Pedro
dc.contributor.authorMartínez Catalán, José R.
dc.contributor.authorArenas, R.
dc.date.accessioned2014-11-19T11:45:12Z
dc.date.available2014-11-19T11:45:12Z
dc.date.issued2002
dc.description.abstractThe Arinteiro massif has a complex structure which includes shear zones, recumbent folds, thrusts and upright folds. Ca-poor amphibolites occur associated with the shear zones, although there is some controversy about the origin of such rocks. Shear zones could act as channel-ways for fluids during deformation, modifying the chemical composition of sheared rocks. Detailed field studies and fabric analysis show a close relationship between the impoverishment in calcium of the Arinteiro massif amphibolites and the ductile shear zones. A model to explain the evolution of Ca-poor amphibolites is proposed in which fluids are channelized by the shear zones, extracting calcium from the normal amphibolites. Moreover, calc-silicate rocks occur far from deformation zones and are considered to be metasomatic products of the interaction between Ca-rich fluids/common amphibolitesen_US
dc.identifier.urihttp://hdl.handle.net/10272/9362
dc.language.isospaen_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.accessRightsopen accessen_US
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherCa-poor amphibolitesen_US
dc.subject.otherCa-metasomatismen_US
dc.subject.otherOrdenes Complexen_US
dc.titleNueva interpretación petrológica y tectónica de las anfibolitas pobres en calcio del antiforme de Arinteiro (NO del Macizo Ibérico). II: Estructura e implicaciones para la génesis de anfibolitas pobres en calcioen_US
dc.titleNew tectonic and petrologic interpretation of a Ca-poor amphibolites occurrence in the Arinteiro antiform (NW Iberian Massif). II: Structure and genetic implications for the Ca-poor amphiboliteseng
dc.typejournal articleen_US
dspace.entity.typePublication

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