Publication:
Dolomitización en sistemas kársticos actuales: el caso de la Cueva de Castañar de Ibor (Cáceres)

dc.contributor.authorMartín-Pérez, Andrea
dc.contributor.authorAlonso-Zarza, Ana María
dc.date.accessioned2023-06-20T12:46:27Z
dc.date.available2023-06-20T12:46:27Z
dc.date.issued2005
dc.description.abstractDeposits of recent dolomite in caves constitute one more setting that provide data in order to get one more approach to the "dolomite problem". The moon-milk deposits of the Castañar de Ibor Cave (Cáceres) include spheroidal dolomite which occurs associated with huntite that grows mostly on fibrous aragonite crystals. This study suggests that dolomite formed in relation to microbial films that developed on the aragonite crystals. Within these films, both dolomite and huntite formed, but also the wide presence of dolomite is due to transformation of huntite which is metastable. Magnesium is provided by the dissolution of Precambrian dolostones on which the cave developed.
dc.description.facultyFac. de Ciencias Geológicas
dc.description.refereedTRUE
dc.description.sponsorshipJunta de Extremadura/UCM
dc.description.statuspub
dc.eprint.idhttps://eprints.ucm.es/id/eprint/60598
dc.identifier.issn1576-5172
dc.identifier.urihttps://hdl.handle.net/20.500.14352/52484
dc.journal.titleGeotemas
dc.language.isospa
dc.page.final71
dc.page.initial67
dc.relation.projectID316/2003
dc.rights.accessRightsopen access
dc.subject.cdu551.435.8
dc.subject.cdu552.5
dc.subject.keywordDolomite
dc.subject.keywordEnvironmental conditions
dc.subject.keywordMoon-milk
dc.subject.keywordCaves
dc.subject.keywordMicrobial films.
dc.subject.ucmGeodinámica
dc.subject.ucmPetrología
dc.subject.unesco2507 Geofísica
dc.titleDolomitización en sistemas kársticos actuales: el caso de la Cueva de Castañar de Ibor (Cáceres)
dc.typejournal article
dc.volume.number8
dspace.entity.typePublication
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