Internal layering structure and subglacial conditions along a traverse line from Zhongshan Station to Dome A, East Antarctica, revealed by ground-based radar sounding-Reference-Cited by-同舟云学术

Internal layering structure and subglacial conditions along a traverse line from Zhongshan Station to Dome A, East Antarctica, revealed by ground-based radar sounding

Published:2020-12 Issue:5-6 Volume:17 Page:870-878
ISSN:1672-7975
Container-title:Applied Geophysics
language:en
Short-container-title:Appl. Geophys.

Author:

Tang Xue-Yuan,Sun Bo,Wang Tian-Tian

Publisher

Springer Science and Business Media LLC

Subject

Geophysics

Link

https://link.springer.com/content/pdf/10.1007/s11770-020-0866-y.pdf

Reference32 articles.

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2. Cui X B, Sun B, Tian G, et al. Preliminary results of ice radar investigation along the traverse between Zhongshan and Dome A in East Antarctic ice sheet: Ice thickness and subglacial topography. Chinese Science Bulletin, 2010, 55(24): 2715–2722.

3. Ding M, Xiao C, Li Y, et al. Spatial variability of surface mass balance along a traverse route from Zhongshan station to Dome A, Antarctica,2011,J. Glaciol., 57,658–666.

4. Drews R, Eisen O, Weikusat I,, et al. Layer disturbances and the radio-echo free zone in ice sheets. Cryosphere, 2009, 3:195–203.

5. Ferraccioli F, Finn C A, Jordan T A,et al. East Antarctic rifting triggers uplift of the Gamburtsev Mountains. Nature,2011, 479(7373):388–392.

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