untitled
<OAI-PMH schemaLocation=http://www.openarchives.org/OAI/2.0/ http://www.openarchives.org/OAI/2.0/OAI-PMH.xsd>
<responseDate>2018-01-15T15:41:10Z</responseDate>
<request identifier=oai:HAL:hal-00411972v1 verb=GetRecord metadataPrefix=oai_dc>http://api.archives-ouvertes.fr/oai/hal/</request>
<GetRecord>
<record>
<header>
<identifier>oai:HAL:hal-00411972v1</identifier>
<datestamp>2018-01-11</datestamp>
<setSpec>type:ART</setSpec>
<setSpec>subject:sdu</setSpec>
<setSpec>subject:sde</setSpec>
<setSpec>collection:CNRS</setSpec>
<setSpec>collection:SDE</setSpec>
<setSpec>collection:GM</setSpec>
<setSpec>collection:GIP-BE</setSpec>
<setSpec>collection:AGROPOLIS</setSpec>
<setSpec>collection:INSU</setSpec>
<setSpec>collection:UNIV-AG</setSpec>
<setSpec>collection:B3ESTE</setSpec>
<setSpec>collection:UNIV-MONTPELLIER</setSpec>
</header>
<metadata><dc>
<publisher>HAL CCSD</publisher>
<title lang=en>Analogue modelling of the interaction between tectonics, erosion and sedimentation in foreland thrust belts</title>
<creator>Graveleau, Fabien</creator>
<creator>Dominguez, Stephane</creator>
<contributor>Géosciences Montpellier ; Université des Antilles et de la Guyane (UAG) - Institut national des sciences de l'Univers (INSU - CNRS) - Université de Montpellier (UM) - Centre National de la Recherche Scientifique (CNRS)</contributor>
<description>International audience</description>
<source>ISSN: 0010-7999</source>
<source>EISSN: 1432-0967</source>
<source>Contributions to Mineralogy and Petrology</source>
<publisher>Springer Verlag</publisher>
<identifier>hal-00411972</identifier>
<identifier>https://hal.archives-ouvertes.fr/hal-00411972</identifier>
<source>https://hal.archives-ouvertes.fr/hal-00411972</source>
<source>Contributions to Mineralogy and Petrology, Springer Verlag, 2008, 340 (5), pp.324-333. 〈10.1016/j.crte.2008.01.005〉</source>
<identifier>DOI : 10.1016/j.crte.2008.01.005</identifier>
<relation>info:eu-repo/semantics/altIdentifier/doi/10.1016/j.crte.2008.01.005</relation>
<language>en</language>
<subject lang=en>analogue modelling</subject>
<subject lang=en>relief</subject>
<subject lang=en>piedmont</subject>
<subject lang=en>tectonics</subject>
<subject lang=en>erosion</subject>
<subject lang=en>climate</subject>
<subject lang=en>accretionary wedges</subject>
<subject lang=en>sandbox experiments</subject>
<subject lang=en>mountain belts</subject>
<subject lang=en>China</subject>
<subject>[SDU.STU.TE] Sciences of the Universe [physics]/Earth Sciences/Tectonics</subject>
<subject>[SDE.MCG] Environmental Sciences/Global Changes</subject>
<type>info:eu-repo/semantics/article</type>
<type>Journal articles</type>
<description lang=en>The structure and dynamic evolution of a mountain belt piedmont are controlled by strong interactions between tectonics, surface processes (erosion, sedimentation), and climate. Studying these couplings relies on detailed geometric and kinematic analysis of morphostructural markers (folds, faults, terraces, alluvial surfaces) and analysis of syntectonic sedimentation. To study quantitatively how these markers form, evolve and record deformation, we developed a new analogue modelling approach using a specific composite granular material. The originality stands in the simultaneous modelling of orogenic deformation mechanisms and erosion-transport-sedimentation processes, but also in the use of techniques allowing quantitative measurement of morphostructural evolution. This methodology opens new perspectives in the fields of geomorphology (relief dynamics), seismotectonics (study of active faults), and sedimentology (including sequential stratigraphy).</description>
<date>2008</date>
</dc>
</metadata>
</record>
</GetRecord>
</OAI-PMH>