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dc.contributor.authorTremul, A.
dc.contributor.authorCalligaris, R.
dc.contributor.authorLenaz, D.
dc.contributor.authorPrincivalle, F.
dc.date.accessioned2010-01-25T09:38:20Z
dc.date.available2010-01-25T09:38:20Z
dc.date.issued2001
dc.identifier.citationCadernos do Laboratorio Xeolóxico de Laxe, 2001, 26: 497-502 ISSN: 00213-4497es_ES
dc.identifier.issn0213-4497
dc.identifier.urihttp://hdl.handle.net/2183/6508
dc.description.abstract[Abstract] In 1999 two borings were performedin the area of Pocala Cave, one outside the cave and the other inside in the cave. In particular four samples of the first boring were studied.It seems that mineralogy is strictly connected with sedimentology where quartz and plagioclase are present. It could be a consequence of a periodical floods of flysch sediments during interglacial period
dc.language.isoenges_ES
dc.publisherUniversidade da Coruñaes_ES
dc.subjectPocala Cavees_ES
dc.subjectBoringses_ES
dc.subjectMineralogyes_ES
dc.subjectStratigraphyes_ES
dc.titlePreliminary report on sediments from Pocala Cave: sedimentological and heavy mineral analysises_ES
dc.title.alternativeEstudio sedimentológico preliminar y análisis de minerales pesados en la cueva Pocala
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.rights.accessinfo:eu-repo/semantics/openAccess


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