Please use this identifier to cite or link to this item:
|Authors: ||D'Amico, S.*|
|Title: ||Seismicity and Focal Mechanisms at the Calabro-Lucanian boundary along the Apennine chain (southern Italy)|
|Title of journal: ||RENDICONTI ONLINE DELLA SOCIETÀ GEOLOGICA ITALIANA|
|Series/Report no.: ||/21 (2012)|
|Issue Date: ||2012|
|Keywords: ||Calabro-Lucanian region|
|Abstract: ||The Calabro-Lucanian boundary is a complex geological zone marking the transition between the highly seismogenic tectonic
domains of Southern Apennines and the Calabrian Arc.
Historical catalogues include earthquakes with macroseismic effects up to VII-VIII MCS (CPTI WORKING GROUP, 2004) and paleoseismological investigations suggested that earthquakes of
magnitude between 6.5 and 7 may have occurred in this area,
between the 6th and the 15th century (MICHETTI et alii, 2000).
More recently, on 9 September 1998, an earthquake of moment
magnitude M5.6 occurred at the north-western margin of the
Pollino massif (GUERRA et alii, 2005; ARRIGO et alii, 2006) and
since the second half of 2010 the same region was interested by a noteworthy seismic activity characterized by several swarms with thousands of events with a maximum magnitude of 3.6.|
|Appears in Collections:||04.06.99. General or miscellaneous|
Papers Published / Papers in press
Files in This Item:
|D'amico el al 2012.pdf||112.46 kB||Adobe PDF||View/Open
Items in DSpace are protected by copyright, with all rights reserved, unless otherwise indicated.