Active tectonics along the Nebrodi-Peloritani boundary in northeastern Sicily (Southern Italy)

被引:19
作者
Pavano, F. [1 ]
Romagnoli, G. [1 ]
Tortorici, G. [1 ]
Catalano, S. [1 ]
机构
[1] Univ Catania, Sez Sci Terra, Dipartimento Sci Biol Geol & Ambientali, I-95129 Catania, Italy
关键词
Active tectonics; Seismotectonic; Tectonic reactivation; Calabrian arc; NE Sicily; SLIP HISTORY; ZONE; ARC; DEFORMATION; EARTHQUAKES; APENNINES;
D O I
10.1016/j.tecto.2015.07.024
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
In the epicentral area of the seismic swarm of the June-September 2011, at southern edge of the Calabrian arc in NE Sicily, very recent extensional motions remobilised two main NW-SE dextral faults. The extensional reactivation of strike-slip faults responded to a new regional dynamic, also evidenced by GPS and seismological data. The inverted structures are aligned at the margin of a wide crustal block that is moving apart from the rest of the island and is uplifting faster than the adjacent regions. The active faults terminate to the northwest at the intersection with a prominent NNE trending fault that represents the western boundary of the mobile block. The vertical displacement along this border exactly matches the difference in elevation of the marine terraces resting inside and outside the block, respectively. On the contrary, only part of differential displacement of the marine terraces was actually accommodated as cumulative motion along the two NW oriented inverted faults, across the southwestern boundary of the block. Amounts of the vertical displacement were distributed on distinct fault planes of the previous dextral shear belts. The widespread fracturing is also the best explanation for the seismic swarm of the 2011, whose epicenters spread on a discrete rock volume rather than concentrated along a single fault plane. The diffuse fracturing seems to represent a peculiar style of deformation, connected to the tectonic inversion of previous strike-slip shear zones. Seismic swarm also affects the northern termination of the Calabrian arc where active extensional deformation reactivated previous strike-slip faults. The similarity of the two regions suggests that seismic swarm can be peculiar of extensional belts developed on previous strike-slip shear zones, along which the pre-existing geometry favours the dispersion of the tectonic motion on a network of small linked fault planes. (C) 2015 Elsevier B.V. All rights reserved.
引用
收藏
页码:1 / 11
页数:11
相关论文
共 48 条
  • [1] Amato A., 1995, ANN GEOPHYS, V38, P255, DOI DOI 10.4401/AG-4122
  • [2] Amidio-Morelli L., 1976, Memorie della Societa Italiana, V17, P1
  • [3] ACTIVE TECTONICS OF THE ADRIATIC REGION
    ANDERSON, H
    JACKSON, J
    [J]. GEOPHYSICAL JOURNAL OF THE ROYAL ASTRONOMICAL SOCIETY, 1987, 91 (03): : 937 - 983
  • [4] [Anonymous], 1991, Il Quaternario
  • [5] Late quaternary paleoclimate in the eastern Mediterranean region from stable isotope analysis of speleothems at Soreq Cave, Israel
    BarMatthews, M
    Ayalon, A
    Kaufman, A
    [J]. QUATERNARY RESEARCH, 1997, 47 (02) : 155 - 168
  • [6] THE ASTRONOMICAL THEORY OF CLIMATE AND THE AGE OF THE BRUNHES-MATUYAMA MAGNETIC REVERSAL
    BASSINOT, FC
    LABEYRIE, LD
    VINCENT, E
    QUIDELLEUR, X
    SHACKLETON, NJ
    LANCELOT, Y
    [J]. EARTH AND PLANETARY SCIENCE LETTERS, 1994, 126 (1-3) : 91 - 108
  • [7] BENAVRAHAM Z, 1995, TECTONOPHYSICS, V243, P57
  • [8] Post-glacial slip history of the Sparta fault (Greece) determined by 36Cl cosmogenic dating:: Evidence for non-periodic earthquakes -: art. no. 1246
    Benedetti, L
    Finkel, R
    Papanastassiou, D
    King, G
    Armijo, R
    Ryerson, F
    Farber, D
    Flerit, F
    [J]. GEOPHYSICAL RESEARCH LETTERS, 2002, 29 (08) : 87 - 1
  • [9] NEW DATA AND HYPOTHESIS ON THE DEVELOPMENT OF THE TYRRHENIAN BASIN
    BOCCALETTI, M
    NICOLICH, R
    TORTORICI, L
    [J]. PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY, 1990, 77 (01) : 15 - 40
  • [10] Bonfiglio L., 1984, Geografia Fisica e Dinamica Quaternaria, V6, P3