Articles | Volume 8, issue 5
Solid Earth, 8, 857–882, 2017
https://doi.org/10.5194/se-8-857-2017
Solid Earth, 8, 857–882, 2017
https://doi.org/10.5194/se-8-857-2017

Research article 05 Sep 2017

Research article | 05 Sep 2017

Earthquake static stress transfer in the 2013 Gulf of Valencia (Spain) seismic sequence

Lluís Saló et al.

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Cited articles

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Aki, K. and Richards, P. G.: Quantitive Seismology: Theory and Methods, University Science Books, USA, 700 pp., 1980.
Allen, C. R.: The tectonic environments of seismically active and inactive areas along the San Andreas fault system, Stanford University Publications, Geological Sciences, 11, 70–80, 1968.
Anderson, E. M.: The dynamics of faulting and dyke formation with applications to Britain, Edinburgh, Oliver and Boyd, 1951.
Baisch, S., Carbon, D., Dannwolf, U., Delacou, B., Devaux, M., Dunand, F., Jung, R., Koller, M., Martin, C., and Sartori, M.: Deep heat mining basel: seismic risk analysis, SERIANEX Group, Departementfür Wirtschaft, Soziales und Umwelt des Kantons Basel-Stadt, Basel, Switzerland, 2009.
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Short summary
Fault movement on the crust is governed by stress levels. Our study focuses on the effect of stress transfer between faults, a mechanism long known to have potential for generating earthquakes. Our results suggest that static stress transfer would have acted as a destabilizing trigger during the sequence and that the experienced events would not have shortened the occurrence of future damaging shakes. The study aims to provide insight on an issue related to energy resources management.