John D. Platt
Carnegie Institution for Science, Washington, DC
Activity
2015
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RAPID DUCTILE AFTERSLIP FROM COSEISMIC HEATING
T173 Strike Slip Fault Systems Transfer Stress Inboard from the Subduction Zone Margin Leading to Basin Subsidence and Orogensis, Are Conduits for Magmatism, and Are Responsible for Far-Traveled Terrane TranslationMonday, 2 November 20151:30 PM - 5:30 PMRoom 308