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Comparative analysis of earthquakes data recorded by the innovative Precision Laser Inclinometer instruments and the classic Hydrostatic Level System

The Hydrostatic Level System (HLS) data and the Precision Laser Inclinometer (PLI) instruments data have been comparatively analyzed in the event of surface angular oscillations induced by earthquakes. The comparative data analysis has shown an agreement on the arrival and stop time of earthquakes....

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Detalles Bibliográficos
Autores principales: Azaryan, N, Batusov, V, Budagov, J, Glagolev, V, Lyablin, M, Trubnikov, G, Shirkov, G, Gayde, J -Ch, Di Girolamo, B, Herty, A, Mainaud Durand, H, Mergelkuhl, D, Rude, V
Lenguaje:eng
Publicado: 2017
Materias:
Acceso en línea:https://dx.doi.org/10.1134/S1547477117030049
http://cds.cern.ch/record/2270103
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author Azaryan, N
Batusov, V
Budagov, J
Glagolev, V
Lyablin, M
Trubnikov, G
Shirkov, G
Gayde, J -Ch
Di Girolamo, B
Herty, A
Mainaud Durand, H
Mergelkuhl, D
Rude, V
author_facet Azaryan, N
Batusov, V
Budagov, J
Glagolev, V
Lyablin, M
Trubnikov, G
Shirkov, G
Gayde, J -Ch
Di Girolamo, B
Herty, A
Mainaud Durand, H
Mergelkuhl, D
Rude, V
author_sort Azaryan, N
collection CERN
description The Hydrostatic Level System (HLS) data and the Precision Laser Inclinometer (PLI) instruments data have been comparatively analyzed in the event of surface angular oscillations induced by earthquakes. The comparative data analysis has shown an agreement on the arrival and stop time of earthquakes. The data have been analyzed within the instruments sensitivity ranges having an overlap in frequency intervals.
id oai-inspirehep.net-1600321
institution Organización Europea para la Investigación Nuclear
language eng
publishDate 2017
record_format invenio
spelling oai-inspirehep.net-16003212019-09-30T06:29:59Zdoi:10.1134/S1547477117030049http://cds.cern.ch/record/2270103engAzaryan, NBatusov, VBudagov, JGlagolev, VLyablin, MTrubnikov, GShirkov, GGayde, J -ChDi Girolamo, BHerty, AMainaud Durand, HMergelkuhl, DRude, VComparative analysis of earthquakes data recorded by the innovative Precision Laser Inclinometer instruments and the classic Hydrostatic Level SystemDetectors and Experimental TechniquesThe Hydrostatic Level System (HLS) data and the Precision Laser Inclinometer (PLI) instruments data have been comparatively analyzed in the event of surface angular oscillations induced by earthquakes. The comparative data analysis has shown an agreement on the arrival and stop time of earthquakes. The data have been analyzed within the instruments sensitivity ranges having an overlap in frequency intervals.oai:inspirehep.net:16003212017
spellingShingle Detectors and Experimental Techniques
Azaryan, N
Batusov, V
Budagov, J
Glagolev, V
Lyablin, M
Trubnikov, G
Shirkov, G
Gayde, J -Ch
Di Girolamo, B
Herty, A
Mainaud Durand, H
Mergelkuhl, D
Rude, V
Comparative analysis of earthquakes data recorded by the innovative Precision Laser Inclinometer instruments and the classic Hydrostatic Level System
title Comparative analysis of earthquakes data recorded by the innovative Precision Laser Inclinometer instruments and the classic Hydrostatic Level System
title_full Comparative analysis of earthquakes data recorded by the innovative Precision Laser Inclinometer instruments and the classic Hydrostatic Level System
title_fullStr Comparative analysis of earthquakes data recorded by the innovative Precision Laser Inclinometer instruments and the classic Hydrostatic Level System
title_full_unstemmed Comparative analysis of earthquakes data recorded by the innovative Precision Laser Inclinometer instruments and the classic Hydrostatic Level System
title_short Comparative analysis of earthquakes data recorded by the innovative Precision Laser Inclinometer instruments and the classic Hydrostatic Level System
title_sort comparative analysis of earthquakes data recorded by the innovative precision laser inclinometer instruments and the classic hydrostatic level system
topic Detectors and Experimental Techniques
url https://dx.doi.org/10.1134/S1547477117030049
http://cds.cern.ch/record/2270103
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