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Speleothem micritization in a vadose meteoric environment (Castañar de Ibor Cave, Cáceres)

dc.contributor.authorMartín García, Rebeca
dc.contributor.authorAlonso Zarza, Ana María
dc.contributor.authorMartín Pérez, Andrea
dc.date.accessioned2014-07-04T08:53:41Z
dc.date.available2014-07-04T08:53:41Z
dc.date.issued2007
dc.identifier.urihttp://hdl.handle.net/10272/8422
dc.description.abstractThe aragonite and calcite speleothems of the Castañar de Ibor Cave show white and matt coatings that formed by micritization and dissolution of the initial crystals. These processes are also recognised in the inner part of the speleothems. Either in the inner or outher parts the result is the lost of brightness and transparency of the speleothems. Petrographically these coatings are seen as lines of micrite liked to dissolution processes that probably occurred because of the circulation of undersaturated fluids within the cave. At the moment no organic structures have been recognised in relation to the micritizated areas, indicating very probably that the process was inorganically drivenen_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.otherMicritizationen_US
dc.subject.otherSpeleothemsen_US
dc.subject.otherAragoniteen_US
dc.subject.otherCalciteen_US
dc.titleMicritización de espeleotemas en ambiente meteórico vadoso (Cueva de Castañar de Ibor, Cáceres)en_US
dc.titleSpeleothem micritization in a vadose meteoric environment (Castañar de Ibor Cave, Cáceres)eng
dc.typeinfo:eu-repo/semantics/articleen_US
dc.rights.accessRightsinfo:eu-repo/semantics/openAccess


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