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What is Seismic Activity in Western Pyrenees about?

The document summarizes new seismic data collected from a temporary seismic network in the western Pyrenees region for 17 months. The key findings are: 1) The seismicity delineates the westward continuation of the E-W trending Pyrenean seismicity belt through the Variscan Basque Massifs along the Leiza Fault, ending at the Hendaya Fault. 2) The seismicity is distributed on a crustal scale, dipping northward to depths of almost 30 km. 3) Other seismic events are related to the central segment of the Pam

Author

Artyom Lebedev

Language

EN