Bin He
Guangzhou Institute of Geochemistry, China Academy of Science, Guangzhou, N/A
Activity
2013
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CONSTRAINING THE CAUSE OF THE END-GUADALUPIAN EXTINCTION WITH COUPLED RECORDS OF CARBON AND CALCIUM ISOTOPES
303 Recent Advances in Paleoclimatology/PaleooceanographyWednesday, 30 October 20138:00 AM - 12:00 PMRoom 605
2011
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CONSTRAINTS ON OCEAN BIOGEOCHEMISTRY DURING THE END-GUADALUPIAN BIOTIC CRISIS FROM STABLE CALCIUM ISOTOPES
T153 Permian-Triassic Changes and Extinction Event: New Insights from Sedimentary, Geochemical, and Paleobiological Records and Modeling Approaches ITuesday, 11 October 20118:00 AM - 12:00 PMRoom 200FG
2009
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HIGH PRECISION U-PB GEOCHRONOLOGY OF THE FANGSHAN PLUTON, BEIJING, CHINA: IMPLICATION FOR THE INCREMENTAL GROWTH OF ZONED PLUTONS
33 Petrology, Igneous (Posters)Sunday, 18 October 20099:00 AM - 6:00 PMHall A
2007
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TERMINATION OF THE EMEISHAN FLOOD VOLCANISM AND RELATIONSHIPS TO THE END-GUADALUPIAN MASS EXTINCTION: SHRIMP DATING OF DETRITAL ZIRCONS FROM THE POST-VOLCANIC XUANWEI FORMATION, SW CHINA
T104 Pulse of the Earth: Geochronology and Paleomagnetism of Large Igneous Provinces, the Key to Reconstructing Precambrian SupercontinentsMonday, 29 October 20071:30 PM - 5:30 PM
Date Unknown
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STRUCTURAL EVIDENCE FOR NESTED DIAPIRS IN THE FANGSHAN PLUTON, CHINA
83 Structural Geology and Tectonics (Posters)
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USING PETROLOGIC AND GEOCHEMICAL EVIDENCE TO TEST INCREMENTAL GROWTH MODELS FOR THE FANGSHAN PLUTON, CHINA
143 Mineralogy/Crystallography; Petrology; Volcanology (Posters)