Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/2894
Authors: Basili, R.* 
Barba, S.* 
Title: Migration and shortening rates in the northern Apennines, Italy: implications for seismic hazard
Other Titles: Migration and shortening rates in the Apennines
Journal: Terra Nova 
Series/Report no.: 6 / 19 (2007)
Publisher: Blackwell-Synergy
Issue Date: Dec-2007
DOI: 10.1111/j.1365-3121.2007.00772.x
URL: http://www.blackwell-synergy.com/doi/pdf/10.1111/j.1365-3121.2007.00772.x
Keywords: Active thrust faults
active folds
thrust belt migration
shortening
earthquakes
Subject Classification04. Solid Earth::04.04. Geology::04.04.01. Earthquake geology and paleoseismology 
04. Solid Earth::04.04. Geology::04.04.09. Structural geology 
04. Solid Earth::04.06. Seismology::04.06.01. Earthquake faults: properties and evolution 
04. Solid Earth::04.07. Tectonophysics::04.07.02. Geodynamics 
04. Solid Earth::04.07. Tectonophysics::04.07.04. Plate boundaries, motion, and tectonics 
04. Solid Earth::04.07. Tectonophysics::04.07.06. Subduction related processes 
04. Solid Earth::04.07. Tectonophysics::04.07.07. Tectonics 
05. General::05.01. Computational geophysics::05.01.04. Statistical analysis 
Abstract: Is compression across the northern Apennine fold-and-thrust system (Italy) still active? To address this question, we quantified the long-term rates of migration and shortening of the system along with the measurement errors. Our approach integrates structural geology, seismicity patterns, and statistical treatment of tectonic activity. On the basis of recently published surface and subsurface data, we found a migration rate of 8.85 ± 0.61 mm/yr. The inception age of individual fold structures follow closely this average rate, indicating that the system has been migrating at a constant rate for the past 17 Myr. Cumulative shortening of the system also increases linearly through time at 2.93 ± 0.31 mm/yr. The location of the youngest structures in the easternmost portion of the system coincides with a significant peak of seismic moment released by historical earthquakes. We conclude that not only these easternmost thrusts are still active, but also that they generate earthquakes.
Appears in Collections:Article published / in press

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