Cristiano Collettini
Università degli Studi di Perugia, Perugia, N/A
Activity
2013
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NANO-SCALE DIFFUSION-ACCOMMODATED WEAKENING TRIGGERED BY FRICTIONAL SLIDING DURING EARTHQUAKES IN CARBONATE ROCKS?
T294 The Rock Record of Fault Rheology and Slip Dynamics IITuesday, 29 October 20131:00 PM - 5:00 PMRoom 506
2010
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INTEGRATED STUDIES OF THE MECHANICS OF WEAK LOW-ANGLE NORMAL FAULTS
T173 Where Does Earthquake Physics Meet Earthquake Geology?Tuesday, 2 November 20108:00 AM - 12:00 PMLobby F
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FLUID OVERPRESSURE AND EARTHQUAKE TRIGGERING on DOLOMITES AND ANHYDRITES BEARING FAULTS: INTEGRATION OF FIELD AND LABORATORY STUDIES
T195 Where Does Earthquake Physics Meet Earthquake Geology? (Posters)Tuesday, 2 November 20108:00 AM - 6:00 PMHall D
2007
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FOOTWALL EXTENSION DURING LOW-ANGLE NORMAL FAULTING: CONTROLS ON FAULT ZONE STRUCTURE AND FAULT ROCK DISTRIBUTION
T17 Reservoirs to Ruptures: Multidisciplinary Approaches to Studying Fault Rock Distribution and Evolution in the Seismogenic CrustSunday, 28 October 20078:00 AM - 12:00 PM
2004
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MICROSEISMICITY ALONG LOW-ANGLE NORMAL FAULTS TRIGGERED BY FLUID OVERPRESSURE: AN EXAMPLE FROM THE ALTOTIBERINA FAULT (CENTRAL ITALY)
T237 Low-angle Normal Faults and Faulting: Field Studies, Fault Rocks, Mechanics, and Weakening MechanismsWednesday, 10 November 20041:30 PM - 5:30 PM
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WEAKENING MECHANISMS ALONG LOW-ANGLE NORMAL FAULTS
T237 Low-angle Normal Faults and Faulting: Field Studies, Fault Rocks, Mechanics, and Weakening MechanismsWednesday, 10 November 20041:30 PM - 5:30 PM