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The Lower Palaeozoic albitites from Western Asturias: possible source of leucogranites?

dc.contributor.authorGarcía Arias, M.
dc.contributor.authorCorretgé Castañón, Luis Guillermo
dc.contributor.authorCastro Dorado, Antonio 
dc.date.accessioned2014-07-17T13:27:48Z
dc.date.available2014-07-17T13:27:48Z
dc.date.issued2006
dc.identifier.urihttp://hdl.handle.net/10272/8578
dc.description.abstractIn the West Asturian-Leonese Zone there are some albititic beds of volcanoclastic origin interlayered in the lower part of the Serie de los Cabos, deposited in a graben-type basin during the Middle Cambrian. The mineralogy is plagioclase (albite), rutile, sheet silicates and sometimes quartz, carbonates and chloriteserpentine cryptocrystalline masses. Melting experiments at 850ºC, 6 kbar and added 10% water conditions produce very silicic melts, with different rates of melting according to quartz percentage, but the fertility of these rocks as sources of leucogranites is very lowen_US
dc.language.isospaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/
dc.subject.otherAlbititeen_US
dc.subject.otherParedesen_US
dc.subject.otherCineritic depositen_US
dc.subject.otherSilicic meltsen_US
dc.titleLas albititas del Paleozoico Inferior del occidente de Asturias: ¿posible fuente de leucogranitos?en_US
dc.titleThe Lower Palaeozoic albitites from Western Asturias: possible source of leucogranites?eng
dc.typeinfo:eu-repo/semantics/articleen_US
dc.rights.accessRightsinfo:eu-repo/semantics/openAccess


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