Achilli, V
(Osservatorio Vesuviano —)
,
Al-Bayari, O
(Napoli, Italy)
,
Artese, G
(DISTART —)
,
Borgstrom, S
(Università)
,
Capone, M
(di Bologna, Italy)
,
Del Gaudio, C
(Università)
,
Gandolfi, S
(dé)
,
Macchiavelli, N
(lla Calabria —)
,
Ricciardi, G.P
(Consenza, Italy)
,
Ricco, C
(Correspondence to: Dr. Sven Borgstrom —)
,
Sepe, V
(Osservatorio Vesuviano, Via A. Manzoni, 249-80123 Naples, Italy.)
,
Vettore, A
(Osservatorio Vesuviano —)
AbstractThe surveillance of the Neapolitan volcanic area (Mt. Vesuvius, the Phlegrean Fields and the island of Ischia) represents the principal activity of the Osservatorio Vesuviano. Such an activity is carried out also through the study of ground deformations. This study deals with the use of the ...
AbstractThe surveillance of the Neapolitan volcanic area (Mt. Vesuvius, the Phlegrean Fields and the island of Ischia) represents the principal activity of the Osservatorio Vesuviano. Such an activity is carried out also through the study of ground deformations. This study deals with the use of the GPS as a powerful topographic technique. In the last two years, three GPS networks in the above mentioned area were established, with 8 vertices at Mt. Vesuvius, 20 vertices in the Island of Ischia and 30 vertices in the Phlegrean Fields. In Mt. Vesuvius area a GPS test was carried out, in order to verify the possibility of the installation of a network of GPS permanent stations. In the island of Ischia, three different GPS techniques (Static, Fast Static and RTK-Real Time Kinematics) have been used to get a first set of coordinates and to carry out a comparison between these in small extension areas. GPS data of the Phlegrean Fields are still in processing. The results for Mt. Vesuvius area and the island of Ischia are hereby presented and discussed.
AbstractThe surveillance of the Neapolitan volcanic area (Mt. Vesuvius, the Phlegrean Fields and the island of Ischia) represents the principal activity of the Osservatorio Vesuviano. Such an activity is carried out also through the study of ground deformations. This study deals with the use of the GPS as a powerful topographic technique. In the last two years, three GPS networks in the above mentioned area were established, with 8 vertices at Mt. Vesuvius, 20 vertices in the Island of Ischia and 30 vertices in the Phlegrean Fields. In Mt. Vesuvius area a GPS test was carried out, in order to verify the possibility of the installation of a network of GPS permanent stations. In the island of Ischia, three different GPS techniques (Static, Fast Static and RTK-Real Time Kinematics) have been used to get a first set of coordinates and to carry out a comparison between these in small extension areas. GPS data of the Phlegrean Fields are still in processing. The results for Mt. Vesuvius area and the island of Ischia are hereby presented and discussed.
참고문헌 (7)
internal report of the Osservatorio Vesuviano A.A.V.V 1998 Rendiconto sull'attivita di sorveglianza dell'Osservatorio Vesuviano
Beutler 1993 Documentation of Bernese Software
Reports on Surveying and Geodesy Crespi 237 1996 A Software Package for the Adjustment and Analysis of GPS Control Networks
Leick 1994 GPS Satellite Surveying
Capra 1992 III Geodetic Meeting Static, Fast-Static and Kinematic Use of GPS Receivers
Hein 115 1995 International Association of Geodesy Symposia High Precision Deformation Monitoring Using Differential GPS
ASPRS/ACSM Sumpter 1994 Real-Time Kinematic GPS For Cadastral Surveys
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