Abstract

2014-05-01 to 2014-05-31
Ambient seismic noise measurements will be applied to detect fluid migration and state changes in the Campi Felgrei caldera. Repeatedly, waveform signals generated by a large number of mini-vibroseis sources will be collected at dense seismic arrays.

Related People

Person Institute
Heiko Woith (PI) GFZ Potsdam

Used Equipment

Device Amount
EDL 5
Cube3 50
Trillium Compact 5
3-D Geophone 74

Location

[40.8273° N, 14.1218° E]

Related Publications and Data