Quaternary glaciation of Muztag Ata and Kongur Shan: Evidence for glacier response to rapid climate changes throughout the Late Glacial and Holocene in westernmost Tibet-Reference-Cited by-同舟云学术

Quaternary glaciation of Muztag Ata and Kongur Shan: Evidence for glacier response to rapid climate changes throughout the Late Glacial and Holocene in westernmost Tibet

Published:2009-02-05 Issue:3-4 Volume:121 Page:348-365
ISSN:0016-7606
Container-title:Geological Society of America Bulletin
language:en
Short-container-title:Geological Society of America Bulletin

Author:

Seong Yeong Bae,Owen Lewis A.,Yi Chaolu,Finkel Robert C.

Publisher

Geological Society of America

Subject

Geology

Reference92 articles.

1. HYDROLOGICAL CYCLES ON THE NORTH AND SOUTH PERIPHERIES OF MOUNTAIN–GLACIAL BASINS OF CENTRAL ASIA

2. The 8k event: cause and consequences of a major Holocene abrupt climate change

3. Holocene climatic instability: A prominent, widespread event 8200 yr ago

4. Millennial-scale climatic oscillations during the last interglaciation in central China

5. 0278-7407(1993)012[1335:HCADRA]2.0.CO;2 Arnaud N.O. Brunel M. Cantagrel J.M. Tapponnier P. 1993, High cooling and denudation rates at Kongur Shan, eastern Pamir (Xinjiang, China) revealed by 40Ar/39Ar alkali feldspar thermochronology: Tectonics, v. 12, p. 1335– 1346, doi: 10.1029/93TC00767.

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