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<datestamp>2018-01-11</datestamp>
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<title lang=en>Impact of erosion, sedimentation, and structural heritage on the structure and kinematics of orogenic wedges: Analog models and case studies</title>
<creator>Malavieille, Jacques</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>orogenic wedges</description>
<source>ISSN: 1052-5173</source>
<source>GSA Today</source>
<publisher>Geological Society of America</publisher>
<identifier>hal-00558931</identifier>
<identifier>https://hal.archives-ouvertes.fr/hal-00558931</identifier>
<source>https://hal.archives-ouvertes.fr/hal-00558931</source>
<source>GSA Today, Geological Society of America, 2010, 20 (1), pp.4-10. 〈10.1130/GSATG48A.1〉</source>
<identifier>DOI : 10.1130/GSATG48A.1</identifier>
<relation>info:eu-repo/semantics/altIdentifier/doi/10.1130/GSATG48A.1</relation>
<language>en</language>
<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>Interaction between surface and tectonic processes plays a key role in the structural evolution, kinematics, and exhumation of rocks in orogenic wedges. The deformation patterns observed in analog models show that strain partitioning has a strong impact on the vertical component of displacement of tectonic units, which in return favors erosion in domains of important uplift. Partitioning is controlled by tectonic processes and by climate-dependent surface processes, including erosion and sedimentation. The effects of partitioning include localization of deformed domains, exhumation above areas of deep underplating, and steady-state maintenance of wedges for long time periods. Simple models illustrate well how the morphostructural evolution of mountain belts is determined by these complex interactions.</description>
<date>2010-01-01</date>
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