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  5. The shallow boreholes at The AltotiBerina near fault Observatory (TABOO; northern Apennines of Italy)
 
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The shallow boreholes at The AltotiBerina near fault Observatory (TABOO; northern Apennines of Italy)

Author(s)
Chiaraluce, Lauro  
Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italia  
Collettini, Cristiano  
Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italia  
Cattaneo, Marco  
Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italia  
Monachesi, Giancarlo  
Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italia  
Language
English
Obiettivo Specifico
2T. Sorgente Sismica
Status
Published
JCR Journal
JCR Journal
Journal
SCIENTIFIC DRILLING  
Issue/vol(year)
/ 17 (2014)
Pages (printed)
31-35
Date Issued
2014
DOI
10.5194/sd-17-31-2014
URI
https://www.earth-prints.org/handle/2122/10870
Subjects
04. Solid Earth::04.06. Seismology::04.06.01. Earthquake faults: properties and evolution  
Subjects

Boreholes

Altotiberina fault

Near Fault Observator...

Abstract
As part of an interdisciplinary research project, funded by the European Research Council and addressing
the mechanics of weak faults, we drilled three 200–250 m-deep boreholes and installed an array of
seismometers. The array augments TABOO (The AltotiBerina near fault ObservatOry), a scientific infrastructure
managed by the Italian National Institute of Geophysics and Volcanology. The observatory, which consists
of a geophysical network equipped with multi-sensor stations, is located in the northern Apennines (Italy) and
monitors a large and active low-angle normal fault.
The drilling operations started at the end of 2011 and were completed by July 2012. We instrumented the
boreholes with three-component short-period (2 Hz) passive instruments at different depths. The seismometers
are now fully operational and collecting waveforms characterised by a very high signal to noise ratio that is
ideal for studying microearthquakes. The resulting increase in the detection capability of the seismic network
will allow for a broader range of transients to be identified.
Type
article
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41-Chiaraluce_EtAl_SD_2014.pdf

Size

2.95 MB

Format

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Checksum (MD5)

a617dbf6e1041201682b9f1326071ec6

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