Zhu Huang
Beijing
Activity
2015
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FORMATION OF OPHIOLITE-HOSTED DIAMONDS BY DEEP SUBDUCTION OF OCEANIC LITHOSPHERE: EVIDENCE FROM MINERAL INCLUSIONS
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