Looking at fault reactivation matching structural geology and seismological data

被引:45
作者
Collettini, C [1 ]
Chiaraluce, L
Pucci, S
Barchi, MR
Cocco, M
机构
[1] Univ Perugia, I-06100 Perugia, Italy
[2] Ist Nazl Geofis & Vulcanol, Rome, Italy
关键词
reactivation; earthquakes; fault zone; Apennines;
D O I
10.1016/j.jsg.2004.10.016
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
We investigate fault reactivation that occurred during the 1997 Colfiorito seismic sequence (central Italy), matching detailed structural geology, precise earthquake locations and mechanical models of fault interaction. The Coltiorito area, within the Northern Apennines, is characterised by a relatively recent inversion of the tectonic stress field from compression (late Miocene), to extension (late Pliocene-Quaternary). In September-October 1997 the area experienced a protracted seismic sequence consisting of six moderate magnitude earthquakes (5 < Mw < 6), that ruptured SW-dipping normal fault segments. The two main ruptures of the sequence show opposite directions of rupture propagation and are segmented by a strike-slip fault inherited from the compressional tectonic phase. Late in the sequence this strike-slip fault nucleated an Mw = 4.3 event and an associated aftershock sequence, which we present as an example of reversal of fault slip direction. Plotting the strike-slip events on a detailed geological map, the left-lateral strike-slip fault imaged by aftershock distribution and focal mechanisms, strictly corresponds to the mapped N10 degrees right-lateral strike-slip structure inherited from the compressional tectonic phase. The two different data-sets for this strike-slip fault show the same geometry but opposite kinematics. We analyse the coseismic elastic static stress changes due to the occurrence of the normal fault events in order to investigate the mechanical coupling and interaction between the NW-SE oriented normal fault system and the intervening N10 degrees inherited fault. We show that the elastic stress perturbation increased on the shallow portion of the activated volume where the N10 degrees structure is located, and promoted its reactivation with a strike-slip motion. The different amount of slip experienced along the two normal faults responsible for the greater mainshocks favoured the left-lateral strike-slip kinematics. (c) 2005 Elsevier Ltd. All rights reserved.
引用
收藏
页码:937 / 942
页数:6
相关论文
共 25 条
[1]  
Barchi M., 1998, Memorie della Societa Geologica Italiana, V52, P383
[2]  
BARCHI MR, 2001, FED IT SCI TERR FIST
[3]  
BARCHI MR, 2000, SINTESI SULLE CONSO
[4]   Active tectonics in the central Apennines and possible implications for seismic hazard analysis in peninsular Italy [J].
Cello, G ;
Mazzoli, S ;
Tondi, E ;
Turco, E .
TECTONOPHYSICS, 1997, 272 (01) :43-68
[5]   Imaging the complexity of an active normal fault system: The 1997 Colfiorito (central Italy) case study [J].
Chiaraluce, L ;
Ellsworth, WL ;
Chiarabba, C ;
Cocco, M .
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH, 2003, 108 (B6)
[6]  
CHIARALUCE L, 1997, TECTONICS, V24
[7]   Static stress changes and fault interaction during the 1997 Umbria-Marche earthquake sequence [J].
Cocco, M ;
Nostro, C ;
Ekström, G .
JOURNAL OF SEISMOLOGY, 2000, 4 (04) :501-516
[8]  
*CTPI, 1999, CAT PAR TERR IT
[9]   Moment tensor analysis of the central Italy earthquake sequence of September-October 1997 [J].
Ekstrom, G ;
Morelli, A ;
Boschi, E ;
Dziewonski, AM .
GEOPHYSICAL RESEARCH LETTERS, 1998, 25 (11) :1971-1974
[10]   The recognition of reactivation during continental deformation [J].
Holdsworth, RE ;
Butler, CA ;
Roberts, AM .
JOURNAL OF THE GEOLOGICAL SOCIETY, 1997, 154 :73-78