Gui-Tang Pan
Chengdu Institute of Geology and Mineral Resources, Chengdu, N/A
Activity
2010
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EARLY CRETACEOUS SUBDUCTION-RELATED ADAKITE-LIKE ROCKS FROM THE SOUTHERN MARGIN OF THE LHASA TERRANE, TIBET: PRODUCTS OF SLAB MELTING AND SUBSEQUENT MELT–PERIDOTITE INTERACTION?
15 Tectonic, magmatic & geomorphic evolution of high plateaus. Part 1Monday, 4 October 20102:30 PM - 4:50 PMSalon C