Granates de la serie Grosularia-uvarovita en cromititas prodiformes del yacimiento Mercedita (Cuba)

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dc.contributor.authorProenza, Joaquín A.
dc.contributor.authorMelgarejo i Draper, J. C.
dc.date.accessioned2017-02-10T13:06:48Z
dc.date.available2017-02-10T13:06:48Z
dc.date.issued1996
dc.description.abstractThe Mercedita chromite podiform deposit is genetically and spatially related to the Moa-Baracoa ophiolite complex (NW Cuba). The ore bodies are crosscuted by veins, filled up by uvarovite with variable amounts of chromiferous clinochlore , calcite, titanite and rutile. Garnets are zoned and display a broad composition comprised between uvarovite and grossular end members. Their andradite content is very low. These garnets were formed by hydrothermal circulation during late episodes of ophiolite emplacement.en_US
dc.identifier.urihttp://hdl.handle.net/10272/13278
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.otherCubaen_US
dc.subject.otherUvaroviteen_US
dc.subject.otherGrossularen_US
dc.subject.otherMicroprobeen_US
dc.subject.otherHydrothermalen_US
dc.subject.otherOphioliteen_US
dc.subject.otherZoningen_US
dc.titleGranates de la serie Grosularia-uvarovita en cromititas prodiformes del yacimiento Mercedita (Cuba)en_US
dc.titleGrossular-uvarovite garnets in podiform chromitite from Mercedita deposit (Cuba)eng
dc.typejournal articleen_US
dspace.entity.typePublication

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Geogaceta -- Nº 20-7, (1996)