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dc.contributor.author
Grosse, Pablo  
dc.contributor.author
Poppe, Sam  
dc.contributor.author
Delcamp, Audray  
dc.contributor.author
van Wyk de Vries, Benjamin  
dc.contributor.author
Kervyn, Matthieu  
dc.date.available
2020-08-12T12:27:50Z  
dc.date.issued
2020-04  
dc.identifier.citation
Grosse, Pablo; Poppe, Sam; Delcamp, Audray; van Wyk de Vries, Benjamin; Kervyn, Matthieu; Volcano growth versus deformation by strike-slip faults: Morphometric characterization through analogue modelling; Elsevier Science; Tectonophysics; 781; 4-2020; 1-14  
dc.identifier.issn
0040-1951  
dc.identifier.uri
http://hdl.handle.net/11336/111515  
dc.description.abstract
Volcanoes display diverse morphologies as a result of the complex interplay of several constructive and destructive processes. Scaled analogue models offer a tool to isolate and characterize the different processes. Here, we investigate the interplay between volcano growth and deformation caused by an underlying strike-slip fault through simple analogue models. In particular, we analyze the morphometry of analogue volcanoes resulting from different growth-to-deformation ratios. Deformation elongates the volcano edifice at an angle of 10-45º from the fault trace along the extensional quadrants and generates a summit graben structure oriented perpendicular to the edifice elongation. The overall steepness of the edifice decreases, but steep slopes are preserved or increased on the lower compressional flanks, commonly related to small avalanches. Growth can partially to totally mask these features depending on the growth rate to strike-slip velocity ratio. The summit graben is easily masked even by low growth rates, whereas edifice elongation has the best preservation potential. Scaling of the experiments suggests that at volcanoes with growth rate (km3/yr) to strike-slip velocity (km/yr) ratios ≤ 3.8 km3/km, deformation features should be clearly preserved, whereas at volcanoes with ratios ≥ 15 km3/km, deformation features should be completely masked. The typical growth rates of volcanoes (0.01 to 1 km3/ka) and the typical velocities of strike-slip faults (1 to 20 mm/yr) suggest that in nature, growth rate to strike-slip velocity ratios can range over 3 orders of magnitude, spanning both types of end-members. Using examples of both active and inactive volcanoes located on strike-slip faults with variable elongation intensities and orientations, we highlight that the analogue models account for some of the morphometric variability observed at volcanoes in nature, although the role of vent distribution can be a key factor.  
dc.format
application/pdf  
dc.language.iso
eng  
dc.publisher
Elsevier Science  
dc.rights
info:eu-repo/semantics/restrictedAccess  
dc.rights.uri
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/  
dc.subject
VOLCANO MORPHOMETRY  
dc.subject
VOLCANO GROWTH  
dc.subject
TECTONIC DEFORMATION  
dc.subject
STRIKE-SLIP FAULT  
dc.subject
ANALOGUE MODEL  
dc.subject.classification
Vulcanología  
dc.subject.classification
Ciencias de la Tierra y relacionadas con el Medio Ambiente  
dc.subject.classification
CIENCIAS NATURALES Y EXACTAS  
dc.title
Volcano growth versus deformation by strike-slip faults: Morphometric characterization through analogue modelling  
dc.type
info:eu-repo/semantics/article  
dc.type
info:ar-repo/semantics/artículo  
dc.type
info:eu-repo/semantics/publishedVersion  
dc.date.updated
2020-08-05T15:19:40Z  
dc.journal.volume
781  
dc.journal.pagination
1-14  
dc.journal.pais
Países Bajos  
dc.journal.ciudad
Amsterdam  
dc.description.fil
Fil: Grosse, Pablo. Fundación Miguel Lillo. Dirección de Geología; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Tucumán; Argentina  
dc.description.fil
Fil: Poppe, Sam. Vrije Universiteit Brussel; Bélgica  
dc.description.fil
Fil: Delcamp, Audray. Vrije Universiteit Brussel; Bélgica  
dc.description.fil
Fil: van Wyk de Vries, Benjamin. Université Clermont Auvergne; Francia  
dc.description.fil
Fil: Kervyn, Matthieu. Vrije Universiteit Brussel; Bélgica  
dc.journal.title
Tectonophysics  
dc.relation.alternativeid
info:eu-repo/semantics/altIdentifier/url/https://www.sciencedirect.com/science/article/abs/pii/S0040195120300949?via%3Dihub  
dc.relation.alternativeid
info:eu-repo/semantics/altIdentifier/doi/https://dx.doi.org/10.1016/j.tecto.2020.228411