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Macroscopic Description of the Fulgurite from Torre de Moncorvo (Portugal)

dc.contributor.authorLozano Fernández, R. P.
dc.contributor.authorGonzález Laguna, Ruth
dc.contributor.authorMartín Crespo, Tomás
dc.date.accessioned2014-07-02T12:24:48Z
dc.date.available2014-07-02T12:24:48Z
dc.date.issued2007
dc.identifier.urihttp://hdl.handle.net/10272/8402
dc.description.abstractThe rocks designated as fulgurites are the result of the action of atmospheric electrical discharges on soils or rocks. This work describes from the macroscopic point of view the Torre de Moncorvo fulgurite, as a first approach to understand the processes that originate these peculiar anecdotal rocks in the field of Petrology. The fulgurite of Torre de Moncorvo is especially interesting due to the magnitude of the formation event inferred by its size. The fulgurite is mainly composed by glassy phases, and unmelted mineral and fragments of host rocks as minor componentsen_US
dc.language.isospaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/
dc.subject.otherFulguriteen_US
dc.subject.otherLightningen_US
dc.subject.otherGlassen_US
dc.subject.otherMeltingen_US
dc.titleDescripción Macroscópica de la Fulgurita de Torre de Moncorvo (Portugal)en_US
dc.titleMacroscopic Description of the Fulgurite from Torre de Moncorvo (Portugal)eng
dc.typeinfo:eu-repo/semantics/articleen_US
dc.rights.accessRightsinfo:eu-repo/semantics/openAccess


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