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|DEEP-TEE Phase 2
The seismological experiment in and around the East Eifel Volcanic Field ( Germany) DEEP-TEE was continued in 2017. Following two unusually deep micro-earthquakes in September 2013 (about 40 km depth) a seismic network was installed to record more local seismic events in order to better understand the seismicity and dynamics of this region in phase I of this experiment. Phase II of DEEP-TEE experiment was motivated due the recordings of several deep low-frequency (DLF) events in this region. Stations of the KIT-GPI (Geophysical Institute at Karlsruhe Institute of Technology) were used during this phase.
|Digital Object Identifier (DOI)
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FDSN Web Services provide a common data access API for seismic data.
|Data will be provided via the FDSN web service at ws.gpi.kit.edu.