Zobrazeno 1 - 9
of 9
pro vyhledávání: '"F. M. Mele"'
Autor:
A. Michelini, L. Margheriti, M. Cattaneo, G. Cecere, G. D'Anna, A. Delladio, M. Moretti, S. Pintore, A. Amato, A. Basili, A. Bono, P. Casale, P. Danecek, M. Demartin, L. Faenza, V. Lauciani, A. G. Mandiello, A. Marchetti, C. Marcocci, S. Mazza, F. M. Mele, A. Nardi, C. Nostro, M. Pignone, M. Quintiliani, S. Rao, L. Scognamiglio, G. Selvaggi
Publikováno v:
Advances in Geosciences, Vol 43, Pp 31-38 (2016)
The Istituto Nazionale di Geofisica e Vulcanologia (INGV) is an Italian research institution, with focus on Earth Sciences. INGV runs the Italian National Seismic Network (Rete Sismica Nazionale, RSN) and other networks at national scale for monit
Externí odkaz:
https://doaj.org/article/4df1e0bf6fbc40a9a0293783b99a6ede
Autor:
G. N. Stavrakakis, F. M. Mele, G. Karantonis, C. Falcone, G. Drakatos, L. Beranzoli, B. Alessandrini
Publikováno v:
Annals of Geophysics, Vol 40, Iss 1 (1997)
We present a tomographic view of the crust and uppermost mantle beneath the Central Mediterranean area obtained from P-wave arrival times of regional earthquakes selected from the ISC bulletin. The P-wave velocity anomalies are obtained using Thurber
Externí odkaz:
https://doaj.org/article/a25e81d9abfe4459bdbd2d7ab885d24f
Publikováno v:
Annals of Geophysics, Vol 38, Iss 2 (1995)
A tomographic experiment was performed in the Italian region using local and regional arrivaI times of p and S seismological phases selected from the Italian National Bulletin in the time interval 1984-1991. We deter- mined a 3-D crustal P-wave veloc
Externí odkaz:
https://doaj.org/article/0ff454fd856244328f14e9faf70fe4b6
Autor:
F M Mele
Publikováno v:
American Journal of Roentgenology. 167:281-282
Publikováno v:
American Journal of Roentgenology. 166:1232-1233
Publikováno v:
Dynamics of Atmospheres and Oceans. 8:41-58
The linear baroclinic instabilities of a basic geostrophic shear flow in a stratified, thermally active ocean are considered, including the β-effect. It is shown that the internal heat production, even if it introduces only minor changes into the ge
Publikováno v:
Il Nuovo Cimento C. 8:937-954
Different ocean models with one or two layers having constant static stability and supporting constant-shear flows, whose directions are allowed to change with depth, are examined in the frame-work of the linear nonzonal baroclinic stability theory a
Autor:
C E, Spencer, F M, Mele
Publikováno v:
Nursing outlook. 17(2)
Publikováno v:
Seismological Research Letters. 86:1383-1392
Online Material: Tables of distance correction terms, corresponding estimation errors, and station residuals. Even though the most reliable and physically consistent definition of the size of an earthquake is the moment magnitude M w, small earthquak