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<datestamp>2018-01-11</datestamp>
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<title lang=en>Interactions between tectonics erosion and sedimentation during the recent evolution of the Alpine orogen : analogue modeling insights</title>
<creator>Bonnet, Cécile</creator>
<creator>Malavieille, Jacques</creator>
<creator>Mosar, J.</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>
<contributor>Université de Fribourg ; University of Fribourg</contributor>
<description>TECTO LITHO</description>
<source>ISSN: 0278-7407</source>
<source>Tectonics</source>
<publisher>American Geophysical Union (AGU)</publisher>
<identifier>hal-00404424</identifier>
<identifier>https://hal.archives-ouvertes.fr/hal-00404424</identifier>
<source>https://hal.archives-ouvertes.fr/hal-00404424</source>
<source>Tectonics, American Geophysical Union (AGU), 2007, 26, pp.TC6016. 〈10.1029/2006TC002048〉</source>
<identifier>DOI : 10.1029/2006TC002048</identifier>
<relation>info:eu-repo/semantics/altIdentifier/doi/10.1029/2006TC002048</relation>
<language>en</language>
<subject lang=en>Alpine orogenic wedge</subject>
<subject lang=en>analogue modeling</subject>
<subject lang=en>tectonics</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>On the basis of a section across the northwestern Alpine wedge and foreland basin, analogue modeling is used to investigate the impact of surface processes on the orogenic evolution. The basis model takes into account both structural and lithological heritages of the wedge. During shortening, erosion and sedimentation are performed to maintain a critical wedge. Frontal accretion leads to the development of a foreland thrust belt; underplating leads to the formation of an antiformal nappe stack in the internal zones. Important volumes of analogue materials are eroded out of the geological record, which in the case of the Alps suggests that the original lengths and volumes may be underestimated. The foreland basin evolves differently depending on the amounts of erosion/sedimentation. Its evolution and internal structuring is governed by the wedge mechanics, thought to be the main controlling mechanism in the development of the Molasse basin in a feedback interaction with surface processes.</description>
<date>2007</date>
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