Condiciones P-T en xenolitos mantélicos de los volcanes la Banya del Boc y el Puig d’Adri (Girona)

dc.contributor.authorOliveras, V.
dc.contributor.authorGalán, Gumer
dc.date.accessioned2014-06-25T08:56:26Z
dc.date.available2014-06-25T08:56:26Z
dc.date.issued2007
dc.description.abstractSeveral thermometers and one barometer are used in order to determine the P-T conditions of type I xenoliths enclosed in alkaline mafic lavas from the Catalan Neogene-Quaternary volcanism. Average temperatures from the different thermometers are similar and higher in harzburgites (1106- 1036º C) than in lherzolites (1043- 867º C), and one pyroxenite shows similar T to harzburgites (1078º C). Low standard deviation for the T estimates reflects equilibrium in most samples for the thermometric reactions. Pressure estimates show high uncertainty, except for few samples, the pyroxenite included, which give consistent values (15.0- 9.6 kbar) within the spinel lherzolite fielden_US
dc.identifier.urihttp://hdl.handle.net/10272/8347
dc.language.isospaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España
dc.rights.accessRightsopen access
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/
dc.subject.otherlherzolitesen_US
dc.subject.otherHarzburgitesen_US
dc.subject.otherPyroxenitesen_US
dc.subject.otherThermometersen_US
dc.subject.otherBarometersen_US
dc.titleCondiciones P-T en xenolitos mantélicos de los volcanes la Banya del Boc y el Puig d’Adri (Girona)en_US
dc.titleP-T conditions of mantle xenoliths from La Banya del Boc and Puig d’Adri volcanoes (Girona)eng
dc.typejournal articleen_US
dspace.entity.typePublication

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