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Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/581

Authors: Cinti, F. R.*
Cucci, L.*
Marra, F.*
Montone, P.*
Title: The 1997 Umbria-Marche (Italy) earthquake sequence: relationship between ground deformation and seismogenic structure
Title of journal: Geophysical Research Letters
Series/Report no.: 7/26 (1999)
Publisher: American Geophysical Union
Issue Date: Apr-1999
URL: http://www.agu.org/pubs/toc/gl/gl/
Keywords: Structural geology
Fractures and faults
Seismology
Seismicity and seismotectonics
Europe
Abstract: A field survey performed during the 1997 Umbria-Marche earthquake sequence led us to recognize ground and pavement ruptures associated with the three largest shocks (M>= 5.7). The ruptures are concentrated in narrow bands that, in part, are on and near previously mapped high-angle normal fauts. The geometry of the ground deformation is consistent with the NE-trending extension indicated by CMT focal solutions of the mainshocks. The distribution of aftershocks suggests that the three mainshocks occurred on ~40 degree SW-dipping normal faults. Geological investigations, modelling of expected coseismic elevation changes, and seismic data, suggest that the surface deformation is not the direct result of primary rupture of faults at depth.
Appears in Collections:Manuscripts
04.04.01. Earthquake geology and paleoseismology
Papers Published / Papers in press

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