Repeating volcano-tectonic earthquakes at Mt. Etna volcano (Sicily, Italy) during 1999-2009

被引:9
作者
Cannata, Andrea [1 ]
Alparone, Salvatore [1 ]
Ursino, Andrea [1 ]
机构
[1] Osservatorio Etneo, Sez Catania, Ist Nazl Geofis & Vulcanol, I-95123 Catania, Italy
关键词
Volcano tectonic earthquakes; Repeating earthquakes; Mt. Etna volcano; Pernicana fault; SOUFRIERE-HILLS-VOLCANO; PERNICANA FAULT SYSTEM; QUASI-STATIC SLIP; 1991-1993; ERUPTION; TEMPORAL-CHANGES; PARKFIELD; EVENTS; JAPAN; FLANK; FORM;
D O I
10.1016/j.gr.2013.02.012
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Repeating volcano-tectonic (VT) earthquakes, taking place at Mt. Etna during 1999-2009, were detected and analyzed to investigate their behavior. We found 735 families amounting to 2479 VT earthquakes, representing similar to 38% of all the analyzed VT earthquakes. The number of VT earthquakes making up the families ranges from 2 to 23. Over 70% of the families comprise 2 or 3 VT earthquakes and only 20 families by more than 10 events. The occurrence lifetime is also highly variable ranging from some minutes to ten years. In particular, more than half of the families have a lifetime shorter than 0.5 day and only similar to 10% longer than 1 year. On the basis of these results, most of the detected families were considered "burst-type", i.e., show swarm-like occurrence, and hence their origin cannot be explained by a temporally constant tectonic loading. Indeed, since the analyzed earthquakes take place in a volcanic area, the rocks are affected not only by tectonic stresses related to the fairly steady regional stress field but also by local stresses, caused by the volcano, such as magma batch intrusions/movements and gravitational loading. We focused on the five groups of families characterized by the longest repeatability overtime, namely high number of events and long lifetime, located in the north-eastern, eastern and southern flanks of the volcano. Unlike the first four groups, which similarly to most of the detected families show swarm-like VT occurrences, group "v", located in the north-eastern sector, exhibits a more "tectonic" behavior with the events making up such a group spread over almost the entire analyzed period. It is clear how both occurrence and slip rates do not remain constant but vary over time, and such changes are time-related to the occurrence of the 2002-2003 eruption. Finally, by FPFIT algorithm a good agreement between directions identified by nodal planes and the earthquake epicentral distribution was generally found. (C) 2013 International Association for Gondwana Research. Published by Elsevier B.V. All rights reserved.
引用
收藏
页码:1223 / 1236
页数:14
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