Quaternary glacier development and the relationship between the climate change and tectonic uplift in the Helan Mountain

Isolated NE-SW stretching the Helan Mountain massif, separating the temperate grassland of the Ordos plateau from the Tenggeli Desert, is a key position of studying the glacier development in west China as well as the coupling conditions of climate change with tectonic uplift. The glacial landforms...

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Bibliographic Details
Published in:Chinese Science Bulletin
Main Authors: Zhang Wei, He MingYue, Li YongHua, Cui ZhiJiu, Wang ZhiLin, Yu Yang
Other Authors: Zhang, W (reprint author), Liaoning Normal Univ, Coll Urban & Environm Sci, Dalian 116029, Peoples R China., Liaoning Normal Univ, Coll Urban & Environm Sci, Dalian 116029, Peoples R China., Peking Univ, Dept Geog, Beijing 100087, Peoples R China.
Format: Journal/Newspaper
Language:English
Published: 科学通报 英文版 2012
Subjects:
Helan Mountain
last glacial cycle
tectonic uplift
equilibrium line
glaciation
PLEISTOCENE GLACIATION
TIANSHAN MOUNTAINS
EQUILIBRIUM-LINE
CENTRAL CHINA
RIVER VALLEY
CHRONOLOGY
PLATEAU
RANGES
TAIWAN
ice core
Online Access:https://hdl.handle.net/20.500.11897/228925
https://doi.org/10.1007/s11434-012-5283-z
Description
Summary:Isolated NE-SW stretching the Helan Mountain massif, separating the temperate grassland of the Ordos plateau from the Tenggeli Desert, is a key position of studying the glacier development in west China as well as the coupling conditions of climate change with tectonic uplift. The glacial landforms and deposits including cirques, peaks, knife-edge ridges, lateral moraines, and terminal moraines distribute above 2800 m a.s.l. in the middle part of the Helan Mountain. This distribution indicates that here was once glaciated during the late Quaternary. Morphology features show a clear sequence of landscape forming events took place throughout the Helan Mountain. Laboratory optically stimulated luminescence (OSL) and accelerator mass spectrometry radiocarbon dating (AMS C-14) results indicate a late history of glacial advance. Late Pleistocene glaciers in the middle part of the Helan Mountain advanced to near their positions at least four times, and the glacial sequences can be assigned as the middle stage of last glacial cycle (MIS3b, 43.2 +/- 4.0 ka), last glacial maximum (LGM, similar to 18 ka), late glacial (12.0 +/- 1.1 ka) and neo-glacial (3.4 +/- 0.3 ka) respectively. Adopting equilibrium line altitude similar to 2980 m of last glacial maximum and the modern theoretical snowline altitude similar to 4724 m as the maximum amplitudes, and the standard marine isotope curve (MIS) as the glacial equilibrium line change since the Gonghe Movement (150 ka), the relationship between the mountain altitude and glacier development is discussed herein. Compared with other environmental indexes such as the loess-paleosol and ice core, conclusions are made that glacier advances in the Helan Mountain during the late Quaternary obviously depended on the coupled control of tectonic uplift of mountain with the climate condition. It is at last glaciation that the mountain reached the altitude above snowline and coupled with the glacial climate. The glacial advances occurred in the early and middle stages of last glacial cycle after the Gonghe Movement. http://gateway.webofknowledge.com/gateway/Gateway.cgi?GWVersion=2&SrcApp=PARTNER_APP&SrcAuth=LinksAMR&KeyUT=WOS:000311497900013&DestLinkType=FullRecord&DestApp=ALL_WOS&UsrCustomerID=8e1609b174ce4e31116a60747a720701 Multidisciplinary Sciences SCI(E) 5 ARTICLE 34 4491-4504 57

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