2026-06-08T23:16:54Zhttps://docta.ucm.es/rest/oai/requestoai:docta.ucm.es:20.500.14352/1021962025-03-18T13:22:49Zcom_20.500.14352_14col_20.500.14352_21
Docta Complutense
author
Pérez López, Raúl
author
Rodríguez Pascua, Miguel Angel
author
Giner Robles, Jorge Luis
author
Calvo Sorando, José Pedro
author
Garduño Monroy, V.H.
author
Israde Alcántara, I.
author
Bischoff, James L.
editor
Lario Gómez, Javier
editor
Silva Barroso, Pablo Gabriel
2024-03-13T14:46:53Z
2024-03-13T14:46:53Z
2007
978-84-7484-201-2
https://hdl.handle.net/20.500.14352/102196
The diffusion equation was formulated to estimate the age of fault scarps. This technique is rather simple, taking into account the degradation of the unconsolidated scarp with the time. The Tobarra-Cordovilla segment consists in a surface rupturing associated to undated paleoearthquakes. This segment configures a graben basin with normal faults affecting Quaternary deposits. Preliminary study of the paleoearthquake indicates a magnitude greater than 5.5. As a primary approach, we have applied the Diffusion Equation in order to delimitate the age interval of occurrence. However, the diffusion constant for such equation (K0) is only calibrated for arid environmental. Therefore, we have introduced a new equation to obtain the K0-value according the fault throw, the erodability and the apparent density of the unconsolidated faulted sediment.
spa
Calibración de la constante de difusión (k0) para la datación de escarpes cosísmicos: aplicación al terremoto de Alborax (Albacete, SE España)
book part
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URL
https://docta.ucm.es/bitstreams/d6d9ff38-0e42-429e-b150-b1f1d57601e6/download
File
MD5
f84b4bc0ba25f849a0d204ef7720073f
207388
application/pdf
Calibración de la constante de difusión (k0) para la datación de escarpes cosísmicos.pdf
URL
https://docta.ucm.es/bitstreams/6fe87981-5739-4ff6-a068-a4fbc72ee4b9/download
File
MD5
a38736ca135631385205cd338b9773f7
10240
text/plain
Calibración de la constante de difusión (k0) para la datación de escarpes cosísmicos.pdf.txt