Mid-late Pleistocene glacial evolution in the Grove Mountains, East Antarctica, constraints from cosmogenic 10Be surface exposure dating of glacial erratic cobbles

2016 ◽  
Vol 145 ◽  
pp. 71-81 ◽  
Author(s):  
Guocheng Dong ◽  
Feixin Huang ◽  
Chaolu Yi ◽  
Xiaohan Liu ◽  
Weijian Zhou ◽  
...  
2009 ◽  
Vol 24 (8) ◽  
pp. 1016-1028 ◽  
Author(s):  
Conradin Zahno ◽  
Naki Akçar ◽  
Vural Yavuz ◽  
Peter W. Kubik ◽  
Christian Schlüchter

2019 ◽  
Author(s):  
Noel L. Potter ◽  
◽  
Joerg M. Schaefer ◽  
George H. Denton ◽  
Aaron E. Putnam ◽  
...  

2004 ◽  
Vol 53 (1) ◽  
pp. 3
Author(s):  
U Abramowski ◽  
B Glaser ◽  
P W Kubik ◽  
R Zech ◽  
W Zech

Landslides ◽  
2018 ◽  
Vol 15 (10) ◽  
pp. 1991-2000 ◽  
Author(s):  
Xavi Gallach ◽  
Ludovic Ravanel ◽  
Markus Egli ◽  
Dagmar Brandova ◽  
Michael Schaepman ◽  
...  

The Holocene ◽  
2017 ◽  
Vol 27 (10) ◽  
pp. 1516-1525 ◽  
Author(s):  
Guocheng Dong ◽  
Weijian Zhou ◽  
Chaolu Yi ◽  
Li Zhang ◽  
Ming Li ◽  
...  

2009 ◽  
Vol 72 (2) ◽  
pp. 229-233 ◽  
Author(s):  
Ping Kong ◽  
David Fink ◽  
Chunguang Na ◽  
Feixin Huang

AbstractGlacial deposits are present at the head of the Ürümqi River valley, Tianshan, Central Asia. 10Be surface exposure ages of 15 boulders from three sites along a 12 km valley transect range from 9 to 21 ka suggesting emplacement by glacial retreat and advance commencing at the global last glacial maximum (LGM) and most likely abating in the early Holocene. Although the age spread for a given locality is not small, perhaps indicating post-depositional reworking, maximum ages per site are either coeval with or are post-LGM and inconsistent with previous pre-LGM electron spin resonance ages.


2009 ◽  
Vol 1 (3) ◽  
Author(s):  
Stefan Winkler

AbstractThis study provides the first attempt to combine terrestrial (in situ) cosmogenic nuclide (10Be) surface exposure dating with Schmidt hammer relative-age dating for the age estimation of Holocene moraines at Strauchon Glacier, Southern Alps, New Zealand. Numerous Schmidt hammer tests enable a multi-ridged lateral moraine system to be related to three late-Holocene ‘Little Ice Age’-type events. On the basis of cosmogenic 10Be ages, those events are dated to c. 2400, 1700, and 1100 years ago. Linear age-calibration curves are constructed in order to relate Schmidt hammer R-values to cosmogenic 10Be ages. The high explanation yielded reveals the causal link between both data sets. The potential of combining both methods in a ‘’multiproxy approach’ is discussed alongside possible future improvements. Terrestrial cosmogenic nuclide dating delivers absolute ages needed as fixed points for Schmidt hammer age-calibration curves. The Schmidt hammer technique can be used to crosscheck the boulder surfaces chosen for surface exposure dating by terrestrial cosmogenic nuclides. It should, therefore, reduce the number of samples necessary and costs.


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