Dromocrone delle onde P dedotte dallo studio del terremoto profondo del basso Tirreno del 3 Gennaio 1960
Main Article Content
Abstract
By means of a statistica! metliod of Caloi-Peronaci, the
author determines the space-time coordinates of the deep earthquake which
took place in the lower Tirrenian sea on Jan. 3, 1960.
Through a series of attemps performed by making the recording times
of the P's intervene in divers station groupings (intermediate, intermediate
and far, intermediate and near), emphasins is given to the utility of the
data of near stations with regard to a better determination of depth and
origin time.
The most probable equations of tlie travel-time curves of the P waves
are worked out, valid up to distances of 30°. The equations thus obtained
make evident anticipations of the order of 2S in the stations of Messina and
Reggio C. with regard to the times foreseen according to tlie Jeffreys and Bullen
tables. The travel-time curves obtained for the group of scandinavian
stations ( 18°,6 ^ A < 30°) shows anticipations from 6 about (Goteborg) to zero.
author determines the space-time coordinates of the deep earthquake which
took place in the lower Tirrenian sea on Jan. 3, 1960.
Through a series of attemps performed by making the recording times
of the P's intervene in divers station groupings (intermediate, intermediate
and far, intermediate and near), emphasins is given to the utility of the
data of near stations with regard to a better determination of depth and
origin time.
The most probable equations of tlie travel-time curves of the P waves
are worked out, valid up to distances of 30°. The equations thus obtained
make evident anticipations of the order of 2S in the stations of Messina and
Reggio C. with regard to the times foreseen according to tlie Jeffreys and Bullen
tables. The travel-time curves obtained for the group of scandinavian
stations ( 18°,6 ^ A < 30°) shows anticipations from 6 about (Goteborg) to zero.
Article Details
How to Cite
FEDERICO, B. (1963) “Dromocrone delle onde P dedotte dallo studio del terremoto profondo del basso Tirreno del 3 Gennaio 1960”, Annals of Geophysics, 16(3), pp. 513–538. doi: 10.4401/ag-5248.
Issue
Section
OLD
Open-Access License
No Permission Required
Istituto Nazionale di Geofisica e Vulcanologia applies the Creative Commons Attribution License (CCAL) to all works we publish.
Under the CCAL, authors retain ownership of the copyright for their article, but authors allow anyone to download, reuse, reprint, modify, distribute, so long as the original authors and source are cited. No permission is required from the authors or the publishers.
In most cases, appropriate attribution can be provided by simply citing the original article.
If the item you plan to reuse is not part of a published article (e.g., a featured issue image), then please indicate the originator of the work, and the volume, issue, and date of the journal in which the item appeared. For any reuse or redistribution of a work, you must also make clear the license terms under which the work was published.
This broad license was developed to facilitate open access to, and free use of, original works of all types. Applying this standard license to your own work will ensure your right to make your work freely and openly available. For queries about the license, please contact ann.geophys@ingv.it.