Rapid Last Glacial Maximum deglaciation in the Indian Himalaya coeval with midlatitude glaciers: New insights from 10 Be‐dating of ice‐polished bedrock surfaces in the Chandra Valley, NW Himalaya-Reference-Cited by-同舟云学术

Rapid Last Glacial Maximum deglaciation in the Indian Himalaya coeval with midlatitude glaciers: New insights from 10 Be‐dating of ice‐polished bedrock surfaces in the Chandra Valley, NW Himalaya

Published:2016-02-22 Issue:4 Volume:43 Page:1589-1597
ISSN:0094-8276
Container-title:Geophysical Research Letters
language:en
Short-container-title:Geophys. Res. Lett.

Author:

Eugster Patricia¹,Scherler Dirk²³,Thiede Rasmus C.¹,Codilean Alexandru T.²⁴,Strecker Manfred R.¹

Affiliation:

1. Institute of Earth and Environmental Science University of Potsdam Potsdam Germany

2. Earth Surface Geochemistry German Research Centre for Geosciences GFZ Potsdam Germany

3. Institute of Geological Sciences Freie University Berlin Berlin Germany

4. Now at School of Earth and Environmental Sciences University of Wollongong Wollongong New South Wales Australia

Funder

German Science Foundation

DFG, Deutsche Forschungsgemeinschaft

DFG

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1002/2015GL066077

Reference54 articles.

1. Exhumation and incision history of the Lahul Himalaya, northern India, based on (U–Th)/He thermochronometry and terrestrial cosmogenic nuclide methods

2. Supplementary material to "Modeling the statistical distributions of cosmogenic exposure dates from moraines"

3. A complete and easily accessible means of calculating surface exposure ages or erosion rates from 10Be and 26Al measurements

4. An ExcelTM spreadsheet program for reconstructing the surface profile of former mountain glaciers and ice caps

5. The role of the Indian summer monsoon and the mid-latitude westerlies in Himalayan glaciation: review and speculative discussion

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