One- and two- dimensional models are equally effective inmonitoring the 
crust’s thermal response to advection bylarge-scale thrusting 
during orogenesis

dc.contributor.author	Alcock, James E.
dc.contributor.author	Martínez Catalán, José Ramón
dc.contributor.author	Arenas Martín, Ricardo
dc.date.accessioned	2023-06-20T00:20:44Z
dc.date.available	2023-06-20T00:20:44Z
dc.date.issued	2011
dc.description.department	Depto. de Mineralogía y Petrología
dc.description.faculty	Fac. de Ciencias Geológicas
dc.description.refereed	TRUE
dc.description.status	pub
dc.eprint.id	https://eprints.ucm.es/id/eprint/17389
dc.identifier.doi	10.1016/j.cageo.2011.02.012
dc.identifier.issn	0098-3004
dc.identifier.officialurl	http://www.journals.elsevier.com/computers-and-geosciences/
dc.identifier.uri	https://hdl.handle.net/20.500.14352/42431
dc.journal.title	Computers & Geosciences
dc.language.iso	eng
dc.page.final	1207
dc.page.initial	1205
dc.publisher	Pergamon-Elsevier
dc.rights.accessRights	open access
dc.subject.cdu	551.24
dc.subject.keyword	Thermal modeling
dc.subject.keyword	One dimensional
dc.subject.keyword	2-dimensional
dc.subject.keyword	Finite difference
dc.subject.keyword	Orogeny
dc.subject.ucm	Petrología
dc.subject.ucm	Geodinámica
dc.subject.unesco	2507 Geofísica
dc.title	One- and two- dimensional models are equally effective inmonitoring the crust’s thermal response to advection bylarge-scale thrusting during orogenesis
dc.type	journal article
dc.volume.number	37
dspace.entity.type	Publication
relation.isAuthorOfPublication	590ee677-786b-4d34-b10b-30b65d1a8d35
relation.isAuthorOfPublication.latestForDiscovery	590ee677-786b-4d34-b10b-30b65d1a8d35

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