1887

Abstract

The Vilariça Fault Zone (VFZ) is one of the major elements of the late Hercynian strike-slip network in the NW Iberia. Geological and geomorphological criteria reveal that the VFZ was reactivated during Meso and Cenozoic times; an historical seismicity record associated to this tectonic structure demonstrates its present day activity (Ribeiro et aI., 1990).

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/content/papers/10.3997/2214-4609-pdb.299.247
1997-11-07
2022-01-16
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609-pdb.299.247
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