Aviso: para depositar documentos, por favor, inicia sesión e identifícate con tu cuenta de correo institucional de la UCM con el botón MI CUENTA UCM. No emplees la opción AUTENTICACIÓN CON CONTRASEÑA
 

TOPO-EUROPE: From Iberia to the Carpathians and analogues

dc.contributor.authorCloetingh, Sierd
dc.contributor.authorGallart, Josep
dc.contributor.authorVicente Muñoz, Gerardo De
dc.contributor.authorMatenco, Liviu
dc.date.accessioned2023-11-27T16:17:12Z
dc.date.available2023-11-27T16:17:12Z
dc.date.issued2010-11-25
dc.descriptionReceived 5 October 2010 / Received in revised form 8 November 2010 / Accepted 17 November 2010 / Available online 25 November 2010. © 2010 Elsevier B.V. All rights reserved. Corresponding author. Tel.: +31 205987300; fax: +31 206462457. / E-mail addresses: sierd.cloetingh@falw.vu.nl (S.Cloetingh), jgallart@ija.csic.es (J. Gallart), gdv@geo.ucm.es (G. de Vicente), liviu.matenco@falw.vu.nl (L. Matenco).
dc.description.abstractEarth Sciences are rapidly changing from largely descriptive to process-oriented disciplines that aim at quantitative models for the reconstruction and forecasting of the complex processes in the Solid Earth. Prediction is highly relevant for the basic needs of humanity: supply of water and resources, protection against natural hazards and control on the environmental degradation of the Earth. Intensive utilization of the human habitat carries largely unknown risks of and makes us increasingly vulnerable. There is an urgent need for scientifically advanced “geo-prediction systems” that can accurately locate subsurface resources and forecast timing and magnitude of natural hazards. The design of such systems is a major multidisciplinary scientific challenge. The quantitative understanding of the Earth has made significant progress in the last few decades. Important ingredients in this process have been the advances made in seismological methods to obtain information on the 3D structure of the mantle and the lithosphere, in the quantitative understanding of the lithospheric processes as well as the recognition of the key role of quantitative sedimentary basin analysis in connecting temporal and spatial scales. Quantitative understanding of the mass transfer by erosion and deposition as well as their feed back with crustal and subcrustal dynamics presents a new frontier in modern Earth sciences. This research bridges investigations on high-resolution, near-surface time scales and the largescale, long-term approaches characteristic for the lithosphere and basin-wide studies. The essential step towards a 4D approach (in space and time) is a direct response to the need for a full incorporation of geological and geophysical constraints in the modelling of solid Earth processes. TOPO-EUROPE is a multidisciplinary international research program that addresses the interaction of processes inherent to the deep Earth (lithosphere and mantle) with surface processes (erosion, climate and sea level), which together shaped the topography of Europe. The objective of this programme is to quantify natural hazards by incorporating data interactive modelling focused on the lithosphere memory and neotectonics, with special attention on the thermo-mechanical structure of the lithosphere, mechanisms controlling large-scale plate boundaries and intraplate deformations, anomalous subsidence and uplift, and links with surface processes and topography evolution.eng
dc.description.departmentDepto. de Geodinámica, Estratigrafía y Paleontología
dc.description.facultyFac. de Ciencias Geológicas
dc.description.refereedTRUE
dc.description.statuspub
dc.identifier.citationCloetingh, Sierd, et al. «TOPO-EUROPE: From Iberia to the Carpathians and Analogues». Tectonophysics, vol. 502, n.o 1-2, abril de 2011, pp. 1-27. DOI.org (Crossref), https://doi.org/10.1016/j.tecto.2010.11.008.
dc.identifier.doi10.1016/j.tecto.2010.11.008
dc.identifier.essn1879-3266
dc.identifier.issn0040-1951
dc.identifier.officialurlhttps://doi.org/10.1016/j.tecto.2010.11.008
dc.identifier.relatedurlhttp://www.journals.elsevier.com/tectonophysics/
dc.identifier.urihttps://hdl.handle.net/20.500.14352/88998
dc.issue.number1-2
dc.journal.titleTectonophysics
dc.language.isoeng
dc.page.final27
dc.page.initial1
dc.publisherElsevier
dc.rights.accessRightsrestricted access
dc.subject.cdu504.4(4)‑047.72
dc.subject.keywordCarpathians
dc.subject.keywordIberian Peninsula
dc.subject.keywordEarth sciences
dc.subject.keywordErosion
dc.subject.keywordStructural geology
dc.subject.keywordSurface topography
dc.subject.keywordBasin analysis
dc.subject.keywordDeformation
dc.subject.keywordEnvironmental degradation
dc.subject.keywordHazard management
dc.subject.keywordIntraplate process
dc.subject.keywordLithosphere
dc.subject.keywordMass transfer
dc.subject.keywordNatural hazard
dc.subject.keywordNeotectonics
dc.subject.keywordPlate boundary
dc.subject.keywordSedimentary basin
dc.subject.keywordSeismology
dc.subject.keywordSubsidence
dc.subject.keywordThermomechanics
dc.subject.keywordUplift
dc.subject.keywordWater resource
dc.subject.keywordWater supply
dc.subject.ucmGeodinámica
dc.subject.ucmHidrología
dc.subject.ucmSismología (Geología)
dc.subject.unesco2506.07 Geomorfología
dc.subject.unesco2506.05 Hidrogeología
dc.subject.unesco2507.05 Sismología y Prospección Sísmica
dc.titleTOPO-EUROPE: From Iberia to the Carpathians and analogues
dc.typejournal article
dc.type.hasVersionVoR
dc.volume.number502
dspace.entity.typePublication
relation.isAuthorOfPublication09af5f8f-e65c-4c2b-8583-c1c43e152589
relation.isAuthorOfPublication.latestForDiscovery09af5f8f-e65c-4c2b-8583-c1c43e152589

Download

Original bundle

Now showing 1 - 1 of 1
Loading...
Thumbnail Image
Name:
1-s2.0-S0040195110004828-main.pdf
Size:
6.51 MB
Format:
Adobe Portable Document Format

Collections