The 1984 Abruzzo earthquake (Italy): an example of seismogenic process controlled by interaction between differently oriented synkinematic faults
- 1 June 2002
- journal article
- Published by Elsevier in Tectonophysics
- Vol. 350 (3) , 237-254
- https://doi.org/10.1016/s0040-1951(02)00118-x
Abstract
No abstract availableThis publication has 34 references indexed in Scilit:
- Earthquake faulting as a structural processPublished by Elsevier ,2003
- The geometry, kinematics and rates of deformation within an en échelon normal fault segment boundary, central ItalyJournal of Structural Geology, 2000
- Active stress map of ItalyJournal of Geophysical Research, 1999
- The 1954 Rainbow Mountain‐Fairview Peak‐Dixie Valley earthquakes: A triggered normal faulting sequenceJournal of Geophysical Research, 1996
- Paleoseismicity of the Ovindoli‐Pezza fault, central Apennines, Italy: A history including a large, previously unrecorded earthquake in the Middle Ages (860–1300 A.D.)Journal of Geophysical Research, 1996
- Trench investigations of the 1915 Fucino earthquake fault scarps (Abruzzo, central Italy): Geological evidence of large historical eventsJournal of Geophysical Research, 1996
- Heat flow in the tectonic provinces crossed by the southern segment of the European GeotraverseTectonophysics, 1995
- Segmentation and the coseismic behavior of Basin and Range normal faults: examples from east-central Idaho and southwestern Montana, U.S.A.Journal of Structural Geology, 1991
- Historical surface faulting in the Basin and Range province, western North America: implications for fault segmentationJournal of Structural Geology, 1991
- Fault-plane solutions and seismicity of the Italian peninsulaTectonophysics, 1985