Figure 1 | Scientific Reports

Figure 1

From: Ultra-thin clay layers facilitate seismic slip in carbonate faults

Figure 1

Geological setting. (a) Geological setting of the Tre Monti Fault and evidence of surface faulting from historical earthquakes in the central Apennines, Italy. Geological map and base map has been drawn using Adobe Illustrator CS5. (b) Simplified geological cross-section through the Tre Monti Fault. Cross-section trace in (a). Cross-section has been drawn using Adobe Illustrator CS5. (c) The study outcrop of the Tre Monti principal fault (Latitude 42°04′34″ N, Longitude 13°29′58″ E). (d) Simplified structural cross-section through the Tre Monti principal fault showing the ultracataclasite above the foliated cataclasite. Cross-section has been drawn using Adobe Illustrator CS5.

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