Francesca Remitti
University of Modena and Reggio Emilia, Modena
Activity
2017
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CAN SUBDUCTION OF SEDIMENTARY MÉLANGES CONTROL THE MECHANICS OF SHALLOW MEGATHRUST?
T322 Polygenetic Mélanges: A Glimpse on Tectono-Sedimentary Recycling in Convergent MarginsWednesday, 25 October 20178:00 AM - 12:00 PMTahoma 5
2014
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STRUCTURE OF THE PLATE BOUNDARY FAULT IN THE JAPAN TRENCH, AND IMPLICATIONS FOR SLIP BEHAVIOUR
T91 Deformation Localization throughout the CrustMonday, 20 October 20148:00 AM - 12:00 PM118
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EVIDENCE FOR CRACKING AND SILICA REDISTRIBUTION AT THE LOWER END OF THE SEISMOGENIC ZONE, KODIAK, ALASKA AND OTAGO, NEW ZEALAND
T2 The Structure of Faults from Top to Bottom: Implication for Fluid Flow, Ore Deposits, and Seismic Hazard ISunday, 19 October 20148:00 AM - 12:00 PM118
2013
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THE THICKNESS OF PLATE BOUNDARY THRUST FAULTS: IMPLICATIONS FOR DEFORMATION MECHANISM AND THE ROCK RECORD OF SUBDUCTION
1 Tectonic Processes that Build the Stratigraphic and Structural Record of Ancient and Modern Convergent MarginMonday, 20 May 20138:00 AM - 12:00 PMSalon A1