@misc{10481/109958,
year = {2020},
url = {https://hdl.handle.net/10481/109958},
abstract = {Earthquakes are a conspicuous manifestation of active
processes in and around the Iberian Peninsula, providing
evidence for active faulting at the plate boundary zone, as
well as across large intraplate areas. An extensive sample
of faulting from many individual structures is provided
through the earthquakes that appear in the geological,
historical and instrumental records. Modern seismic
broadband networks allow for estimating earthquake
source parameters routinely. The distribution of hypocenters
locates the zones of principal stress release, and focal
mechanism depict the variety of different tectonic regimes
over the region. Older earthquakes have been studied
from paleoseismology, macroseismic information or
analogue recordings, improving our understanding of
long-term characteristics.},
publisher = {Springer Nature},
keywords = {Seismicity},
keywords = {Iberia},
title = {Seismicity of the Iberian Peninsula},
doi = {10.1007/978-3-030-10931-8_3},
author = {Stich, Daniel and Martínez-Solares, José Manuel and Custodio, Susana and Batlló, Josep and Martín, Rosa and Teves-Costa, Paula and Morales Soto, José},
}