Gravity monitoring of active volcanoes is nowadays performed mainly through relative measurements carried out using calibrated spring gravimeters and on networks covering the surveyed area. Networks must be linked to stable reference stations located outside but not so far from the volcanic area. Gravity monitoring of active volcanoes is nowadays performed mainly through relative measurements carried out using calibrated spring gravimeters and on networks covering the surveyed area. Networks must be linked to stable reference stations located outside but not so far from the volcanic area. An uncertainty below 10 μGal can be reached only after applying complex and time consuming field procedures
An in fieri outdoor absolute gravimeter / Germak, ALESSANDRO FRANCO LIDIA; Berrino, G; Carmisciano, C; D'Agostino, G; Sgherri, R.. - (2009), p. 4. (Intervento presentato al convegno II Convegno Nazionale Metodi Gravimetrico, Magnetico, Elettrico ed Elettromagnetico in Sismologia e Vulcanologia tenutosi a Napoli, Italy nel 27-29 ottobre 2009).
An in fieri outdoor absolute gravimeter
GERMAK, ALESSANDRO FRANCO LIDIA;D'AGOSTINO G;
2009
Abstract
Gravity monitoring of active volcanoes is nowadays performed mainly through relative measurements carried out using calibrated spring gravimeters and on networks covering the surveyed area. Networks must be linked to stable reference stations located outside but not so far from the volcanic area. Gravity monitoring of active volcanoes is nowadays performed mainly through relative measurements carried out using calibrated spring gravimeters and on networks covering the surveyed area. Networks must be linked to stable reference stations located outside but not so far from the volcanic area. An uncertainty below 10 μGal can be reached only after applying complex and time consuming field proceduresI documenti in IRIS sono protetti da copyright e tutti i diritti sono riservati, salvo diversa indicazione.
