Active normal faulting during the 1997 seismic sequence in Colfiorito, Umbria: Did slip propagate to the surface?
نویسندگان
چکیده
منابع مشابه
The Depth of Seismic Faulting and the Upper Transition from Stable to Unstable Slip Regimes
A number of observations indicate that an upper stability transition occurs along well-developed faults, such as the San Andreas, as a result of unconsolidated gouge within shallow regions of these faults. These observations include the depth distribution of seismicity along faults with and without well-developed gouge zones, correlations between seismicity and shallow crustal structure, and mo...
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ژورنال
عنوان ژورنال: Journal of Structural Geology
سال: 2016
ISSN: 0191-8141
DOI: 10.1016/j.jsg.2016.08.011