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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
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