Chao Yuan
Guanzhou Institute of Geochemistry, Chinese Academy of Science, Guangzhou, N/A
Activity
2014
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THE ALTAI MOUNTAINS IN CHINA, MONGOLIA AND RUSSIA: A CONTINUOUS SUBDUCTION SYSTEM IN THE EARLY PALEOZOIC
T328 Magmatism, Tectonics, and Metallogeny of the Central Asian Orogenic BeltWednesday, 22 October 20141:00 PM - 5:00 PM118
2009
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U–PB AND HF ISOTOPIC STUDY OF ZIRCONS FROM GNEISSIC ROCKS FROM THE CHINESE ALTAI: IMPLICATIONS FOR PALEOZOIC RIDGE SUBDUCTION?
T60 Lithospheric Delamination, Continental Magmatism, and Crustal Uplift in Mountain EvolutionSunday, 18 October 20091:30 PM - 5:30 PME147/148