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dc.contributor.authorPeral, Mireia
dc.contributor.authorRuh, Jonas
dc.contributor.authorZlotnik, Sergio
dc.contributor.authorFuniciello, Francesca
dc.contributor.authorFernandez Ortiga, Manel
dc.contributor.authorVergés Masip, Jaume
dc.contributor.authorGerya, Taras
dc.contributor.otherUniversitat Politècnica de Catalunya. Departament d'Enginyeria Civil i Ambiental
dc.date.accessioned2021-01-25T12:58:47Z
dc.date.available2021-01-25T12:58:47Z
dc.date.issued2020-06-01
dc.identifier.citationPeral, M. [et al.]. Analog and numerical experiments of double subduction systems with opposite polarity in adjacent segments. "Geochemistry geophysics geosystems", 1 Juny 2020, vol. 21, núm. 6, p. 1-22.
dc.identifier.issn1525-2027
dc.identifier.urihttp://hdl.handle.net/2117/335922
dc.description.abstractIn this work we study the dynamics of double subduction systems with opposite polarity in adjacent segments. A combined approach of numerical and analog experiments allows us to compare results and exploit the strengths of both methodologies. High-resolution numerical experiments complement laboratory results by providing quantities difficult to measure in the laboratory such as stress state, flow patterns, and energy dissipation. Results show strong asymmetries in the mantle flow that produce in turn asymmetries in the trench and in the downgoing slab deformation. The mantle flow pattern varies with time; the toroidal cells between the plates evolve until merging into one unique cell when the trenches align. In that moment the maximum upward flow is observed close to the trenches. The interaction between the mantle flow produced by each subducting plate makes the rollback processes slower than in a single subduction case. This is consistent with the observed energy dissipation rate that is smaller in the double subduction system than in two single subductions. Moreover, we provide a detailed analysis on the setup and boundary conditions required to numerically reproduce the analog experiments. Boundary conditions at the bottom of the domain are crucial to reproduce their analog counterparts. Numerical results are compared to natural examples of multi-slab subduction systems in terms of upper mantle seismic anisotropy, relative trench retreat velocities, and composition of subduction-related magmatism.
dc.format.extent22 p.
dc.language.isoeng
dc.subjectÀrees temàtiques de la UPC::Matemàtiques i estadística::Anàlisi numèrica::Mètodes numèrics
dc.subject.lcshStrength of materials
dc.subject.othermantle flow/plate interaction
dc.subject.othernumerical and analog models
dc.subject.othertrench retreat
dc.subject.othertrench curvature
dc.subject.otherplate deformation
dc.titleAnalog and numerical experiments of double subduction systems with opposite polarity in adjacent segments
dc.typeArticle
dc.subject.lemacResistència de materials
dc.contributor.groupUniversitat Politècnica de Catalunya. LACÀN - Mètodes Numèrics en Ciències Aplicades i Enginyeria
dc.identifier.doi10.1029/2020GC009035
dc.description.peerreviewedPeer Reviewed
dc.subject.amsClassificació AMS::74 Mechanics of deformable solids::74S Numerical methods
dc.subject.amsClassificació AMS::74 Mechanics of deformable solids::74H Dynamical problems
dc.relation.publisherversionhttps://agupubs.onlinelibrary.wiley.com/doi/abs/10.1029/2020GC009035
dc.rights.accessOpen Access
local.identifier.drac29389922
dc.description.versionPostprint (author's final draft)
dc.relation.projectidinfo:eu-repo/grantAgreement/EC/H2020/777778/EU/Multiscale Inversion of Porous Rock Physics using High-Performance Simulators: Bridging the Gap between Mathematics and Geophysics/MATHROCKS
dc.relation.projectidinfo:eu-repo/grantAgreement/MICINN/1PE/DPI2017-85139-C2-2-R
local.citation.authorPeral, M.; Ruh, J.; Zlotnik, S.; Funiciello, F.; Fernandez, M.; Vergés, J.; Gerya, T.
local.citation.publicationNameGeochemistry geophysics geosystems
local.citation.volume21
local.citation.number6
local.citation.startingPage1
local.citation.endingPage22


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