Relocalización de terremotos y sismotectónica mediante un nuevo modelo cortical 3D en el área de la Falla de Alhama de Murcia (SE Iberia)

  1. J.L. Sańchez-Roldán 1
  2. J.J. Martínez-Díaz 1
  3. J.V. Cantavella 2
  4. J.A. Álvarez-Gómez 1
  5. J. Morales 3
  1. 1 Universidad Complutense de Madrid
    info

    Universidad Complutense de Madrid

    Madrid, España

    ROR 02p0gd045

  2. 2 Instituto Geográfico Nacional
    info

    Instituto Geográfico Nacional

    Madrid, España

    ROR https://ror.org/03yycdv57

  3. 3 Instituto de Andaluz de Geofísica
Mostra les afiliacions +
Revista:
Geotemas (Madrid)

ISSN: 1576-5172

Any de publicació: 2021

Títol de l'exemplar: X Congreso Geológico de España

Número: 18

Pàgines: 853

Tipus: Article

DIALNET GOOGLE SCHOLAR lock_openAccés obert editor

Altres publicacions en: Geotemas (Madrid)

Resum

The Eastern Betics Shear Zone comprises one of the most active tectonic areas in Iberia due to the convergence between Eurasia and Africa (Martínez-Díaz et al., 2012). We focus our study in the Alhama de Murcia Fault and other nearby faults, that are the source of large paleoseismic events and some damaging series in the historical period. The study aims to give more accurate locations to the hypocentres in the region. This was accomplished by adding data of events recorded by the Andalusian Seismic Institute (IAG) network, and another local temporal network to the one used in the Spanish Catalogue (IGN) for computing a relocation of those events using a new 3D crustal model of the area, created combining recent geophy- sical data both regional and local (e.g. Díaz and Gallart, 2009; Mancilla and Díaz, 2015). New locations, which reduce the uncertainties of their spatial distribution, allow relating series of events to known fracture families.

Fuente de los datos: Dialnet