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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1998
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| LEADER | 09279caa a22008417a 4500 | ||
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| 001 | PAPER-2856 | ||
| 003 | AR-BaUEN | ||
| 005 | 20241209090744.0 | ||
| 008 | 190411s1998 xx ||||fo|||| 00| 0 eng|d | ||
| 024 | 7 | |2 scopus |a 2-s2.0-0031658048 | |
| 040 | |a Scopus |b spa |c AR-BaUEN |d AR-BaUEN | ||
| 100 | 1 | |a Cernadas, Daniel Carlos | |
| 245 | 1 | 0 | |a Self-similarity in the seismicity of the South-American subduction zone |
| 260 | |c 1998 | ||
| 270 | 1 | 0 | |m Dto. Fisica-Fac. Ciencias Exactas/N., Universidad de Buenos Aires, Ciudad Universitaria, Pab., 1-1428 Buenos Aires, Argentina |
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| 504 | |a Whitman, D., Moho Geometry beneath the Eastern Margin of the Andes, Northwest Argentina, and its Implications to the Effective Elastic Thickness of the Andean Foreland (1994) J. Geophys. Res, 99, pp. 15277-15289 | ||
| 504 | |a Wigger, P., Schmitz, M., Araneda, M., Asch, G., Baldzhun, S., Giese, P., Heinsohn, W., Viramonfte, J., (1993) Variation of the Crustal Structure of the Southern Central Andes, pp. 23-48. , eds. Reutter, K., Scheuber, E., and Wigger, J. (Springer-Verlag, New York) | ||
| 506 | |2 openaire |e Política editorial | ||
| 520 | 3 | |a 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. |l eng | |
| 536 | |a Detalles de la financiación: Consejo Nacional de Investigaciones Científicas y Técnicas | ||
| 536 | |a Detalles de la financiación: Universidad de Buenos Aires | ||
| 536 | |a Detalles de la financiación: This work was partially supported by Consejo Nacional de Investigaciones Científicas y Técnicas, Fundación Antorchas and Universidad de Buenos Aires. | ||
| 593 | |a Dto. Fisica-Fac. Ciencias Exactas/N., Universidad de Buenos Aires, Ciudad Universitaria, Pab., 1-1428 Buenos Aires, Argentina | ||
| 593 | |a Dto. de Sismología, Fac. Cie. Astronomicas/Geofisicas, Universidad de La Plata, Paseo del Bosque, La Plata, Argentina | ||
| 593 | |a Consejo Nac. de Invest. Cie./Tec. | ||
| 651 | 4 | |a SOUTH AMERICA | |
| 690 | 1 | 0 | |a EARTHQUAKE |
| 690 | 1 | 0 | |a FRACTAL ANALYSIS |
| 690 | 1 | 0 | |a SEISMICITY |
| 690 | 1 | 0 | |a SUBDUCTION ZONE |
| 700 | 1 | |a Osella, A. | |
| 700 | 1 | |a Sabbione, N. | |
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