Vickie Bennett
Australian National University, Canberra
Activity
2020
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DIVERSITY IN EOARCHEAN METAMORPHISMS FROM ULTRA-HIGH-PRESSURE TO LOW-PRESSURE (<250 TO >1000°C/GPA) EXPLAINED BY PLATE MOVEMENTS IN DEEP TIME
4 Assembling Laurentia: Turning Points in the Geologic Evolution of the North American ContinentMonday, 26 October 20201:30 PM - 5:30 PMAuditorium
2018
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SOURCES AND TIMING OF THE MINIMUM-MELT MOLE GRANITE, NEW ENGLAND OROGEN, NSW AUSTRALIA
T66 Different Personalities of Granites and Rhyolites: Silicic Magmas from the Lower Crust to the Surface II—A Session in Honor of Calvin Miller, Recipient of the MGPV Distinguished Geological Career AwardSunday, 4 November 20181:30 PM - 5:30 PMRoom 240-241
2017
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MELT INCLUSIONS IN FORSTERITIC OLIVINE FROM HISTORICAL KILAUEA LAVAS REVEAL DIVERSE MANTLE MELT COMPOSITIONS
T208 Petrology across the Inner Solar System: In Honor of Roebling Medalist Ed StolperTuesday, 24 October 20178:00 AM - 12:00 PMSkagit 4
2011
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TEMPORAL, ISOTOPIC AND SPATIAL RELATIONS OF EARLY PALEOZOIC GONDWANA-MARGIN ARC MAGMATISM, CENTRAL TRANSANTARCTIC MOUNTAINS, ANTARCTICA
T11 Linking Modern and Ancient OrogensSunday, 9 October 20118:00 AM - 12:00 PMRoom 200FG
2005
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THE LATE ARCHEAN BIOSPHERIC EXPLOSION
T52 Terrestrial and Extraterrestrial Environments for Microbial Survival ISunday, 16 October 20051:30 PM - 5:30 PM