Please use this identifier to cite or link to this item: https://accedacris.ulpgc.es/jspui/handle/10553/105814
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dc.contributor.authorPerez Torrado, F. J.en_US
dc.date.accessioned2021-03-16T13:05:46Z-
dc.date.available2021-03-16T13:05:46Z-
dc.date.issued1988en_US
dc.identifier.urihttps://accedacris.ulpgc.es/handle/10553/105814-
dc.description.abstractn the studied area, three deformation phases are established. The second one produces the principal observed schistosity. The metamorphic conditions start with a medium metamorphic degree. They continue until tardy to post-phase 3 stages, and then, new conditions of high metamorphic degree with production of new paragenesis are established. Toe plutonic intrusions start in pre to syn-phase2 stages, but the larger volume and granitic diversity coincides or is lightly posterior to high degree metamorphic conditions.en_US
dc.languagespaen_US
dc.sourceII Congreso Geológico de España : Granada, 27 de junio - 1 de julio de 1988, v.2, p. 51-54en_US
dc.subject250601 Geología regionalen_US
dc.subject.otherRocas metamórficasen_US
dc.titleCaracterísticas de los materiales metamórficos y graníticos al W y SW de Bohoyo (Provincia de Ávila)en_US
dc.typeinfo:eu-repo/semantics/conferenceobjecten_US
dc.typeConferenceObjecten_US
dc.relation.conferenceII Congreso Geológico de Españaen_US
dc.description.lastpage54en_US
dc.description.firstpage51en_US
dc.relation.volume2en_US
dc.investigacionCienciasen_US
dc.type2Actas de congresosen_US
dc.description.numberofpages4en_US
dc.utils.revisionen_US
dc.identifier.ulpgcen_US
dc.contributor.buulpgcBU-BASen_US
item.grantfulltextopen-
item.fulltextCon texto completo-
crisitem.author.deptGIR IUNAT: Geología de Terrenos Volcánicos-
crisitem.author.deptIU de Estudios Ambientales y Recursos Naturales-
crisitem.author.deptDepartamento de Física-
crisitem.author.orcid0000-0002-4644-0875-
crisitem.author.parentorgIU de Estudios Ambientales y Recursos Naturales-
crisitem.author.fullNamePérez Torrado, Francisco José-
Appears in Collections:Actas de congresos
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