Xian-Hua Li
Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing
Activity
2020
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THE TRANSITION FROM WITHIN-PLATE TO CONVERGENT MARGIN MAGMATISM IN EAST GONDWANA AT THE DAWN OF THE CRYOGENIAN PERIOD: U-PB, HF AND O ISOTOPE RATIOS IN ZIRCON FROM THE BEMARIVO DOMAIN, NORTH MADAGASCAR
T142 Mapping, Minerals, and Metamorphism—Work Small, Think Big II: A Tribute to the Life of Peter RobinsonWednesday, 28 October 20201:30 PM - 5:30 PMMeeting Rooms
2019
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CAUSE AND CONSEQUENCES OF FLAT-SLAB SUBDUCTION AND FOUNDERING: A SOUTH CHINA EXAMPLE
T140 Present-Day and Ancient Flat-Slab Subduction in Rock Records, Geophysical Images, and Geodynamic ModelsMonday, 23 September 20191:30 PM - 5:30 PMRoom 132ABC, North Building
2018
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NEW ZIRCON U-PB GEOCHRONOLOGY ON THE STURTIAN DEGLACIATION IN SOUTH CHINA
T12 EARTHTIMEs and EarthRates: Exploring the Tempo and Mode of Earth-System Processes and EvolutionSunday, 4 November 20188:00 AM - 12:00 PMRoom 143-144
2015
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A METEORIC WATER COMPONENT TO ORE FORMING FLUIDS IN PORPHYRY COPPER SYSTEMS: EVIDENCE FROM SIMS OXYGEN ISOTOPE ANALYSIS
206 Economic Geology (Posters)Tuesday, 3 November 20159:00 AM - 6:30 PMExhibit Hall
2006
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WHAT FLAT-SLAB SUBDUCTIONS CAN DO: AN EXAMPLE FROM MESOZOIC SOUTH CHINA
15 T3. Shallowing and Steepening Subduction Zones IVFriday, 7 April 20068:30 AM - 12:30 PM