In-situ rock shattering and strain localization along a seismogenic fault in dolostones (Monte Marine fault, Italian Central Apennines)
Author:
Funder
H2020 Euratom
University of Parma
Cariparma Foundation
ERC
Publisher
Elsevier BV
Reference126 articles.
1. Dynamic fracturing by successive coseismic loadings leads to pulverization in active fault zones;Aben;J. Geophys. Res. Solid Earth,2016
2. Coseismic damage generation and pulverization in fault zones: insights from dynamic Split‐Hopkinson Pressure Bar experiments in Thomas, M.Y;Aben,2017
3. Architecture and deformation mechanism of a basin-bounding normal fault in Mesozoic platform carbonates, central Italy;Agosta;J. Struct. Geol.,2006
4. Chert nodules in pelagic limestones as paleo-stress indicators: a 3D geomechanical analysis;Antonellini;J. Struct. Geol.,2020
5. Size-dependent comminution, tectonic mixing, and sealing behavior of a structurally oversimplified”fault zone in poorly lithified sands: evidence for a coseismic rupture?;Balsamo;Geol. Soc. Am. Bull.,2011
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