The Friuli (NE-Italy) tilt/strain gauges and short term observations

The tilt/strainmeter network of the Department of Earth Sciences of the University of Trieste, has by now a long history of records, the Trieste Grotta Gigante horizontal pendulum station having been set up in 1959 and the Friuli tilt/strainmeter stations in 1977. Since then the stations have been c...

Full description

Bibliographic Details
Main Author: C. Braitenberg
Format: Article
Language:English
Published: Istituto Nazionale di Geofisica e Vulcanologia (INGV) 1999-06-01
Series:Annals of Geophysics
Subjects:
Online Access:http://www.annalsofgeophysics.eu/index.php/annals/article/view/3745
id doaj-9261f8a9d73545cc8990ae457c4570bf
record_format Article
spelling doaj-9261f8a9d73545cc8990ae457c4570bf2020-11-24T22:26:43ZengIstituto Nazionale di Geofisica e Vulcanologia (INGV)Annals of Geophysics1593-52132037-416X1999-06-0142410.4401/ag-3745The Friuli (NE-Italy) tilt/strain gauges and short term observationsC. BraitenbergThe tilt/strainmeter network of the Department of Earth Sciences of the University of Trieste, has by now a long history of records, the Trieste Grotta Gigante horizontal pendulum station having been set up in 1959 and the Friuli tilt/strainmeter stations in 1977. Since then the stations have been continuously recording the strain-rate in one of the most seismic areas of the Alpine arc, giving invaluable information on crustal deformation in a tectonically active area. Although maintaining essentially the same mechanical features from the time of installation, the instrumentation has undergone modernization, in order to apply recent technical developments to the network. This regards mainly data acquisition, which now, except for one station, is digital. The data are all available and are stored in the Deformation-Database of the Department of Earth Sciences. At first a description of the essential technical and mechanical properties of the instrumentation constituting the network is given. The mean power spectrum of all instruments covering five decades is presented, which is a powerful means to compare the quality of different stations. Following theoretical considerations of the expected pre- or coseismic deformation accompanying local events, the observations of those events is presented, which ought to give the greatest signals. The coseismic steps are modeled for those events for which a fault plane solution was available.http://www.annalsofgeophysics.eu/index.php/annals/article/view/3745tiltmeterstrainmetershort term observations
collection DOAJ
language English
format Article
sources DOAJ
author C. Braitenberg
spellingShingle C. Braitenberg
The Friuli (NE-Italy) tilt/strain gauges and short term observations
Annals of Geophysics
tiltmeter
strainmeter
short term observations
author_facet C. Braitenberg
author_sort C. Braitenberg
title The Friuli (NE-Italy) tilt/strain gauges and short term observations
title_short The Friuli (NE-Italy) tilt/strain gauges and short term observations
title_full The Friuli (NE-Italy) tilt/strain gauges and short term observations
title_fullStr The Friuli (NE-Italy) tilt/strain gauges and short term observations
title_full_unstemmed The Friuli (NE-Italy) tilt/strain gauges and short term observations
title_sort friuli (ne-italy) tilt/strain gauges and short term observations
publisher Istituto Nazionale di Geofisica e Vulcanologia (INGV)
series Annals of Geophysics
issn 1593-5213
2037-416X
publishDate 1999-06-01
description The tilt/strainmeter network of the Department of Earth Sciences of the University of Trieste, has by now a long history of records, the Trieste Grotta Gigante horizontal pendulum station having been set up in 1959 and the Friuli tilt/strainmeter stations in 1977. Since then the stations have been continuously recording the strain-rate in one of the most seismic areas of the Alpine arc, giving invaluable information on crustal deformation in a tectonically active area. Although maintaining essentially the same mechanical features from the time of installation, the instrumentation has undergone modernization, in order to apply recent technical developments to the network. This regards mainly data acquisition, which now, except for one station, is digital. The data are all available and are stored in the Deformation-Database of the Department of Earth Sciences. At first a description of the essential technical and mechanical properties of the instrumentation constituting the network is given. The mean power spectrum of all instruments covering five decades is presented, which is a powerful means to compare the quality of different stations. Following theoretical considerations of the expected pre- or coseismic deformation accompanying local events, the observations of those events is presented, which ought to give the greatest signals. The coseismic steps are modeled for those events for which a fault plane solution was available.
topic tiltmeter
strainmeter
short term observations
url http://www.annalsofgeophysics.eu/index.php/annals/article/view/3745
work_keys_str_mv AT cbraitenberg thefriulineitalytiltstraingaugesandshorttermobservations
AT cbraitenberg friulineitalytiltstraingaugesandshorttermobservations
_version_ 1725751990492856320