Zobrazeno 1 - 10
of 67
pro vyhledávání: '"C. Carmisciano"'
Autor:
F. Greco, C. Del Negro, A. Esposito, M. Anzidei, P. Stefanelli, C. Carmisciano, F. Caratori Tontini, L. Cocchi, R. Napoli
Publikováno v:
Annals of Geophysics, Vol 51, Iss 1, Pp 25-38 (2008)
In this paper we show and discuss the results of gravity and magnetic surveys of Panarea Island and its archipelago. The most recent volcanic manifestation occurred in November 2002 with a shallow submarine gas eruption between the islets of Dattilo,
Externí odkaz:
https://doaj.org/article/5213f7e1eb884b4c813aab5268ea6792
Autor:
F. Fidecaro, N. Beverini, L. Cocchi, F. Caratori Tontini, C. Carmisciano, P. Stefanelli, D. Embriaco
Publikováno v:
Annals of Geophysics, Vol 51, Iss 5-6, Pp 877-886 (2008)
The site of the European Gravitational Observatory (EGO) located in the countryside near Pisa (Tuscany, Italy) was investigated by a microgravity vertical gradient (MVG) survey. The EGO site houses the VIRGO interferometric antenna for gravitational
Externí odkaz:
https://doaj.org/article/5251987edce04587bcb3685082d4cbb6
Publikováno v:
Annals of Geophysics, Vol 51, Iss 1, Pp 87-103 (2008)
We analyse a microgravity data set acquired from two spring LaCoste & Romberg gravity meters operated in parallel at the same site on Etna volcano (Italy) for about two months (August September 2005). The high sampling rate acquisition (2Hz) allowed
Externí odkaz:
https://doaj.org/article/007c77cb8cd34d5499f6529b79cd6bd4
Publikováno v:
Annals of Geophysics, Vol 50, Iss 3, Pp 397-406 (2007)
Reliability of high resolution airborne and shipborne magnetic surveys depends on accurate removal of temporal variations from the recorded total magnetic field intensity data. At mid latitudes, one or a few base stations are typically located with
Externí odkaz:
https://doaj.org/article/0eea805a42394c2b8b6b3d78d13d693c
Autor:
S. Monti, P. Lusiani, M. Grassi, M. Ciminale, C. Carmisciano, F. Caratori Tontini, P. Stefanelli
Publikováno v:
Annals of Geophysics, Vol 49, Iss 6 (2006)
Recently two marine magnetic surveys, combined with the use of a multi-beam sonar (Kongsberg Marittime EM 300 multibeam: 30 KHz frequency echosounder for hydrographic purposes; acoustic lobe composed of 128 beams able to cover a 150° sector) a side-
Externí odkaz:
https://doaj.org/article/25b3a8fc927c47aa8d2bbea97c688bac
Publikováno v:
Annals of Geophysics, Vol 47, Iss 5 (2004)
This paper presents the revised aeromagnetic anomaly map of Italy and its surrounding seas, projected at reference altitude of 2500 m and geomagnetic epoch 1979.0. The magnetic data set used for the map compilation is composed of the total intensity
Externí odkaz:
https://doaj.org/article/e0de6e31f1534294a0483c781a5adfa0
Publikováno v:
Annals of Geophysics, Vol 46, Iss 3 (2003)
The aim of this work is the formulation of a 3D model of the Mt. Amiata volcanic complex (Southern Tuscany) by means of geomagnetic data. This work is shown not only as a real test to check the validity of the inversion algorithm, but also to add i
Externí odkaz:
https://doaj.org/article/d9925f8c3db0478b8ce4db47eecd2748
Publikováno v:
Annals of Geophysics, Vol 43, Iss 5 (2000)
Magnetic observations made onshore the Italian Peninsula, and across the adjacent seas, have been compiled in a new digital database that provides the first complete regional scale view of the crustal scale magnetic anomalies of the region at sea lev
Externí odkaz:
https://doaj.org/article/09d4bde1ea564e71a1b86ae2fa439936
Autor:
A. Donati, E. Simeone, M. Francesconi, E. Maccioni, E. Alzetta, C. Carmisciano, O. Faggioni, N. Beverini, F. Strumia
Publikováno v:
Annals of Geophysics, Vol 41, Iss 3 (1998)
We present here a project for the industrial development of a new magnetometer that is intended to achieve the highest performance in measuring geomagnetic field. The instrument is based on the well-known technology of optically pumped alkali vapour
Externí odkaz:
https://doaj.org/article/abc4f55348c3419f8235b6d0ad28e561
Publikováno v:
Annals of Geophysics, Vol 41, Iss 3 (1998)
Two main plutonic facies characterize the intrusive complex of the Island of Giglio, and the trend of their contact at depth has been modelled using a 2D½ analysis based on a detailed geomagnetic survey in order to verify the geological hypothesis o
Externí odkaz:
https://doaj.org/article/08d2a2641c354f03af33b942e370aac7