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Genesis of ultrabasic-basic rocks ('Ophiolites') of north Hungary

dc.contributor.authorKubovics, Imre
dc.date.accessioned2018-11-28T11:58:01Z
dc.date.available2018-11-28T11:58:01Z
dc.date.issued1982-07
dc.descriptionInternational Symposium on the Activity of Oceanic Volcanoes. Ponta Delgada, 4-9 August 1980.en
dc.description.abstractMost of the researchers consider the ultrabasic-basic magmatites of North Hungary (Bükk Mountains) to be an ophiolitic complex. Nevertheless, on basis of the comparative analyses of the igneous formations with the typical (South-European, from Asia Minor, etc.) ophiolites, considerable petrological-petrogenetic difference can be established. The most characteristic difference shown in the change of FeO+/MgO as a function .of silica. Dissimilarly of the typical ophiolites, the FeO+/MgO ratio decreases parallel and unambiguously with the increase of silica. Its highest value found within the given sequence in certain ultrabasites (3 to 4). The oxidation degree is also considerably lower than in the ophiolites cited. […].en
dc.description.versioninfo:eu-repo/semantics/publishedVersionpt_PT
dc.identifier.citationKUBOVICS, Imre (1982). Genesis of ultrabasic-basic rocks (‘Ophiolites’) of north Hungary. "Arquipélago. Série Ciências da Natureza", 3: 251-252.pt_PT
dc.identifier.urihttp://hdl.handle.net/10400.3/4893
dc.language.isoengpt_PT
dc.publisherUniversidade dos Açorespt_PT
dc.subjectGeologyen
dc.subjectOphioliteen
dc.subjectBükk Mountainsen
dc.subjectHungaryen
dc.titleGenesis of ultrabasic-basic rocks ('Ophiolites') of north Hungaryen
dc.typejournal article
dspace.entity.typePublication
oaire.citation.conferencePlacePonta Delgada, Açorespt_PT
oaire.citation.endPage252pt_PT
oaire.citation.startPage251pt_PT
oaire.citation.titleArquipélago. Série Ciências da Naturezapt_PT
oaire.citation.volume3pt_PT
rcaap.rightsopenAccesspt_PT
rcaap.typearticlept_PT

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