GLACIER ADVANCES SINCE THE MIS3B(?) IN TIBET AND NEIGHBORING MOUNTAINS BASED ON RADIOCARBON DATINGS

2005 Salt Lake City Annual Meeting (October 16–19, 2005)
Paper No. 15-7

Presentation Time: 9:45 AM-10:00 AM

GLACIER ADVANCES SINCE THE MIS3B(?) IN TIBET AND NEIGHBORING MOUNTAINS BASED ON RADIOCARBON DATINGS
YI, Chaolu, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Shuangqing Road 18, Beijing, 100085, China, clyi@itpcas.ac.cn, OWEN, Lewis A., Geology, University of Cincinnati, Cincinnati, OH 45221, LIU, Kexin, Institute of Heavy Ion Physics, Peking Univ & Key Lab of Heavy Ion, Beijing, 100871, China, and CUI, Zhijiu, Department of Urban Planning and Environmental Sciences, Peking University, Beijing, 100871 More numerical dating data of Quaternary glaciations in wide areas of Tibetan plateau are necessary to understand the paleoglacial climatic dynamic in the plateau. We have dated and collected 67 data of radiocarbon dating and found five Quaternary glacier advances at 40~56ka, 24~16ka, 11.5~10.4ka, 3.1ka, 2.8~2.5ka and Little Ice Age. Few data suggest MIS3b was present in southwestern Tibet, indicating that there might be a strong wet current flowing from India ocean to southwestern Tibet.
2005 Salt Lake City Annual Meeting (October 16–19, 2005) General Information for this Meeting
Presentation Handout (.pdf format, 1812.0 kb)
Session No. 15 Timing and Nature of Mountain Glacier Advances throughout the Last Glacial Cycle Salt Palace Convention Center: 150 ABC 8:00 AM-12:00 PM, Sunday, 16 October 2005 Geological Society of America Abstracts with Programs, Vol. 37, No. 7, p. 40
© Copyright 2005 The Geological Society of America (GSA), all rights reserved. Permission is hereby granted to the author(s) of this abstract to reproduce and distribute it freely, for noncommercial purposes. Permission is hereby granted to any individual scientist to download a single copy of this electronic file and reproduce up to 20 paper copies for noncommercial purposes advancing science and education, including classroom use, providing all reproductions include the complete content shown here, including the author information. All other forms of reproduction and/or transmittal are prohibited without written permission from GSA Copyright Permissions.