Structural features of Panarea volcano in the frame of the Aeolian Arc (Italy): Implications for the 2002-2003 unrest

被引:9
作者
Acocella, Valerio [1 ]
Neri, Marco [2 ]
Walter, Thomas R. [3 ]
机构
[1] Dip Sc Geol Roma Tre, I-00146 Rome, Italy
[2] Ist Nazl Geofis & Vulcanol, Sez Catania, I-95123 Catania, Italy
[3] Deutsches Geoforschungszentrum GFZ Potsdam, Dept Phys Earth, D-14473 Potsdam, Germany
关键词
Arc volcanoes; Extension; Unrest; SOUTHERN TYRRHENIAN SEA; ISLANDS; TECTONICS; EVOLUTION; STROMBOLI; LIPARI; ZONE;
D O I
10.1016/j.jog.2009.01.004
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
070403 [天体物理学]; 070902 [地球化学];
摘要
Panarea, characterized by gas unrest in 2002-2003, is the volcanic island with the least constrained structure in the eastern-central Aeolian Arc (Italy). Based on structural measurements, we define here its deformation pattern relative to the Arc. The main deformations are subvertical extension fractures (63% of data), normal faults (25%) and dikes (12%). The mean orientation of the extension fractures and faults is similar to N38 degrees E, with a mean opening direction of N135 degrees +/- 8 degrees, implying extension with a moderate component of dextral shear. These data, matched with those available for Stromboli volcano (pure opening) and Vulcano, Lipari and Salina volcanoes (predominant dextral motions) along the eastern-central Arc, suggest a progressive westward rotation of the extension direction and an increase in the dextral shear. The dextral shear turns into compression in the western arc. The recent unrest at Panarea, coeval to that of nearby Stromboli, may also be explained by the structural context, as both volcanoes lie along the portion of the Arc subject to extension. (C) 2009 Elsevier Ltd. All rights reserved.
引用
收藏
页码:288 / 292
页数:5
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