Publication:
Los granates del tramo del núcleo de la Sierra de los Santos (Córdoba)

dc.contributor.authorPérez Lorente, F.
dc.contributor.authorArana Castillo, Rafael
dc.contributor.otherFacultad de Ciencias (Química y Matemáticas)en_EN
dc.coverage.spatialEspañaen_EN
dc.date.accessioned2009-09-29T16:50:32Z
dc.date.available2009-09-29T16:50:32Z
dc.date.issued1983
dc.description.abstractThe Sierra de los Santos (Sierra Morena, prov. of Córdoba) consists of precambric and paleozoic materials, essentially chloritic schists, limestones and small outcrops of acid and basic igneous rocks. The garnets studied in this work are the only relict minerals from the first metamorphism process developped in this área. X-ray, optical and chemical data of these garnets are reported. They correspond to the piralspite series; finally, metamorphism conditions having given birth to the garnets are discussed.en_EN
dc.formatapplication/pdfes
dc.format.extent14en_EN
dc.identifier.issn0212-9728
dc.identifier.urihttp://hdl.handle.net/10201/5671
dc.languagespaen_EN
dc.publisherMurcia : Universidad, Servicio de Publicacionesen_EN
dc.relation.ispartofAnales de la Universidad de Murcia, Ciencias, vol. 41, 1983en_EN
dc.rightsinfo:eu-repo/semantics/openAccesses
dc.subjectGeologíaen_EN
dc.subject.otherCDU::5 - Ciencias puras y naturales::55 - Geología. Meteorologíaen_EN
dc.titleLos granates del tramo del núcleo de la Sierra de los Santos (Córdoba)en_EN
dc.typeinfo:eu-repo/semantics/articleen_EN
dspace.entity.typePublicationes
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