Please use this identifier to cite or link to this item: http://hdl.handle.net/10553/10101
DC FieldValueLanguage
dc.contributor.authorVidal Romaní, J. R.en_US
dc.contributor.authorYepes, Jorgeen_US
dc.contributor.authorFernández Mosquera, D.en_US
dc.contributor.authorDe Uña, D.en_US
dc.contributor.authorTwidale, C. R.en_US
dc.date.accessioned2013-05-14T05:00:21Z-
dc.date.accessioned2018-06-15T09:17:39Z-
dc.date.available2013-05-14T05:00:21Z-
dc.date.available2018-06-15T09:17:39Z-
dc.date.issued2004en_US
dc.identifier.urihttp://hdl.handle.net/10553/10101-
dc.description.abstractGranite is emplaced deep in the Earth's crust. It cools and crystallises and is subjected to thermal and magmatic events, and to recurrent stresses. It develops textures or fabrics as well as strain patterns which, as erosion brings the rock mass near the surface, find expression in various fracture sets and systems.es
dc.formatapplication/pdfes
dc.languageengen_US
dc.rightsby-nc-ndes
dc.sourceBinghamton International Geomorphology Symposium (35º.2004. Kentuky): Weathering and landscape evolution: abstracts, p. 31en_US
dc.subject250607 Geomorfologíaes
dc.titleRock of agesen_US
dc.typeinfo:eu-repo/semantics/conferenceobjecten_US
dc.typeConference posteren_US
dc.identifier.absysnet625749-
dc.investigacionCienciases
dc.rights.accessrightsinfo:eu-repo/semantics/openAccesses
dc.type2Póster de congresosen_US
dc.identifier.ulpgces
item.grantfulltextopen-
item.fulltextCon texto completo-
crisitem.author.deptGIR IOCAG:Geología Aplicada y Regional-
crisitem.author.deptIU de Oceanografía y Cambio Global-
crisitem.author.deptDepartamento de Ingeniería Civil-
crisitem.author.orcid0000-0001-5039-1482-
crisitem.author.parentorgIU de Oceanografía y Cambio Global-
crisitem.author.fullNameYepes Temiño, Jorge-
Appears in Collections:Póster de congreso
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