Models of passive margin inversion: implications for the Rhenohercynian fold-and-thrust belt, Belgium and Germany

dc.contributor.authorVanbrabant, Y
dc.contributor.authorBraun, Jean
dc.contributor.authorJongmans, D
dc.date.accessioned2015-12-13T23:24:25Z
dc.date.issued2002
dc.date.updated2015-12-12T09:20:25Z
dc.description.abstractPositive tectonic inversion is related to the transmission of compressional stresses along a décollement into the foreland of an orogenic zone. This stress and strain concentration in regions remote from the main orogenic front is commonly related to the
dc.identifier.issn0012-821X
dc.identifier.urihttp://hdl.handle.net/1885/92216
dc.publisherElsevier
dc.sourceEarth and Planetary Science Letters
dc.subjectKeywords: finite element method; fold and thrust belt; numerical model; passive margin; strain partitioning; stress; tectonic evolution; Belgium; Germany Finite element analysis; Fold and thrust belts; Numerical models; One-dimensional models; Rhenohercynian; Strain; Tectonics
dc.titleModels of passive margin inversion: implications for the Rhenohercynian fold-and-thrust belt, Belgium and Germany
dc.typeJournal article
local.bibliographicCitation.lastpage29
local.bibliographicCitation.startpage15
local.contributor.affiliationVanbrabant, Y, Catholic University of Leuven
local.contributor.affiliationBraun, Jean, College of Physical and Mathematical Sciences, ANU
local.contributor.affiliationJongmans, D, Universite Joseph Fourier
local.contributor.authoremailrepository.admin@anu.edu.au
local.contributor.authoruidBraun, Jean, u8901439
local.description.embargo2037-12-31
local.description.notesImported from ARIES
local.description.refereedYes
local.identifier.absfor040313 - Tectonics
local.identifier.ariespublicationMigratedxPub23236
local.identifier.citationvolume202
local.identifier.doi10.1016/S0012-821X(02)00751-3
local.identifier.scopusID2-s2.0-0037200409
local.identifier.uidSubmittedByMigrated
local.type.statusPublished Version

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