John F. Dewey
Oxford, Oxford
Activity
2017
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GROWTH OF THE NORTH CHINA CRATON BY ARCHEAN THROUGH PALEOPROTEROZOIC ACCRETIONARY OROGENESIS
T181 Cratonic Assembly in the Precambrian: Forming the Core of Modern and Ancient Landmasses (Posters)Monday, 23 October 20179:00 AM - 6:30 PMHalls 4EF
2015
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PLATE ACCRETION OF THE ORDOVICIAN BAY OF ISLANDS OPHIOLITE AND HOT SUBDUCTION/SUBCRETION DURING THE EVOLUTION OF A FORE-ARC R-TR-TR TRIPLE JUNCTION AS THE TACONIC ARC ENCROACHED UPON LAURENTIA
T81 Bridging Two Continents: Diamonds, Zircons and Native Elements in the Mantle: New Discoveries and Models on the Properties and Petrogenesis of Oceanic Mantle LithosphereMonday, 2 November 20158:00 AM - 12:00 PMRoom 347/348
2011
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GEO-EDUCATION IN OUR UNIVERSITIES: A GLOBAL COMPARISON AND SOME LOOKING PROBLEMS
23 Earth Sciences for Society, Education in Earth Sciences and Geoheritage ITuesday, 6 September 201111:00 AM - 4:45 PMA 119
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TRANSTENSION IN THE BRITTLE FIELD: THE EASTERN CALIFORNIA SHEAR ZONE
14 Significance of Large Strike-slip Fault Systems — Active and AncientMonday, 5 September 20112:00 PM - 5:10 PMA 017
2009
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THE OPHIOLITE PARADOX RESOLVED?
268 Tectonics: Advances in Understanding Tectonics and Orogenesis Ancient and ModernWednesday, 21 October 20091:30 PM - 5:30 PMA107/108/109
2006
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TECTONIC SIGNIFICANCE OF THE CARIBBEAN PLATE AS A REFERENCE FRAME SINCE XMA: THE “BACKBONE” EXPLAINED
17 T1. Plenary III: The Backbone of the Americas and Other RegionsFriday, 7 April 20062:00 PM - 6:00 PM