| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 6445092 | Journal of Structural Geology | 2012 | 16 Pages |
Abstract
⺠The Borcola Pass Fault Zone (BPFZ) is a strike-slip fault zone cutting dolomitic host rocks. ⺠The damage zone of the BPFZ is cut by secondary faults exploiting pre-existing joints. ⺠Microstructures of dolostone-cutting slip zones suggest coseismic fluidization. ⺠Structural complexity of the BPFZ is comparable with that of active seismogenic faults cutting carbonates.
Keywords
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geology
Authors
Michele Fondriest, Steven A.F. Smith, Giulio Di Toro, Dario Zampieri, Silvia Mittempergher,