Self-similarity in the seismicity of the South-American subduction zone

The spatial distribution of hypocenters corresponding to intermediate and deep seismicity along the South-American subduction zone has led to a description of the geometry of this subduction process. Changes in the angle of subduction have been detected, which led to a division of the subducted regi...

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Autores principales: Cernadas, D., Osella, A., Sabbione, N.
Formato: JOUR
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Acceso en línea:http://hdl.handle.net/20.500.12110/paper_00334553_v152_n1_p57_Cernadas
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spelling todo:paper_00334553_v152_n1_p57_Cernadas2023-10-03T14:45:42Z Self-similarity in the seismicity of the South-American subduction zone Cernadas, D. Osella, A. Sabbione, N. earthquake fractal analysis seismicity subduction zone South America The spatial distribution of hypocenters corresponding to intermediate and deep seismicity along the South-American subduction zone has led to a description of the geometry of this subduction process. Changes in the angle of subduction have been detected, which led to a division of the subducted region into segments according to the flat or normal dipping of the oceanic slab. In this paper the seismicity corresponding to the different segments is analyzed in order to determine the kind of correlation with the slab configuration. Spatial analyses using a multifractal technique are performed and the self-similar behavior is quantified through the fractal dimension. Scale-invariant clusterings, with a high correlation between the spatial fractaldimension and the dipping angle of subduction have been found. Fil:Cernadas, D. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. Fil:Osella, A. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. JOUR info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by/2.5/ar http://hdl.handle.net/20.500.12110/paper_00334553_v152_n1_p57_Cernadas
institution Universidad de Buenos Aires
institution_str I-28
repository_str R-134
collection Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA)
topic earthquake
fractal analysis
seismicity
subduction zone
South America
spellingShingle earthquake
fractal analysis
seismicity
subduction zone
South America
Cernadas, D.
Osella, A.
Sabbione, N.
Self-similarity in the seismicity of the South-American subduction zone
topic_facet earthquake
fractal analysis
seismicity
subduction zone
South America
description The spatial distribution of hypocenters corresponding to intermediate and deep seismicity along the South-American subduction zone has led to a description of the geometry of this subduction process. Changes in the angle of subduction have been detected, which led to a division of the subducted region into segments according to the flat or normal dipping of the oceanic slab. In this paper the seismicity corresponding to the different segments is analyzed in order to determine the kind of correlation with the slab configuration. Spatial analyses using a multifractal technique are performed and the self-similar behavior is quantified through the fractal dimension. Scale-invariant clusterings, with a high correlation between the spatial fractaldimension and the dipping angle of subduction have been found.
format JOUR
author Cernadas, D.
Osella, A.
Sabbione, N.
author_facet Cernadas, D.
Osella, A.
Sabbione, N.
author_sort Cernadas, D.
title Self-similarity in the seismicity of the South-American subduction zone
title_short Self-similarity in the seismicity of the South-American subduction zone
title_full Self-similarity in the seismicity of the South-American subduction zone
title_fullStr Self-similarity in the seismicity of the South-American subduction zone
title_full_unstemmed Self-similarity in the seismicity of the South-American subduction zone
title_sort self-similarity in the seismicity of the south-american subduction zone
url http://hdl.handle.net/20.500.12110/paper_00334553_v152_n1_p57_Cernadas
work_keys_str_mv AT cernadasd selfsimilarityintheseismicityofthesouthamericansubductionzone
AT osellaa selfsimilarityintheseismicityofthesouthamericansubductionzone
AT sabbionen selfsimilarityintheseismicityofthesouthamericansubductionzone
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