Journal cover Journal topic
The Cryosphere An interactive open-access journal of the European Geosciences Union
Journal topic

Journal metrics

Journal metrics

  • IF value: 4.790 IF 4.790
  • IF 5-year value: 5.921 IF 5-year
    5.921
  • CiteScore value: 5.27 CiteScore
    5.27
  • SNIP value: 1.551 SNIP 1.551
  • IPP value: 5.08 IPP 5.08
  • SJR value: 3.016 SJR 3.016
  • Scimago H <br class='hide-on-tablet hide-on-mobile'>index value: 63 Scimago H
    index 63
  • h5-index value: 51 h5-index 51
Volume 12, issue 2
The Cryosphere, 12, 491–504, 2018
https://doi.org/10.5194/tc-12-491-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
The Cryosphere, 12, 491–504, 2018
https://doi.org/10.5194/tc-12-491-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.

Research article 08 Feb 2018

Research article | 08 Feb 2018

Crustal heat production and estimate of terrestrial heat flow in central East Antarctica, with implications for thermal input to the East Antarctic ice sheet

John W. Goodge
Viewed  
Total article views: 1,304 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
804 475 25 1,304 19 35
  • HTML: 804
  • PDF: 475
  • XML: 25
  • Total: 1,304
  • BibTeX: 19
  • EndNote: 35
Views and downloads (calculated since 14 Aug 2017)
Cumulative views and downloads (calculated since 14 Aug 2017)
Viewed (geographical distribution)  
Total article views: 1,216 (including HTML, PDF, and XML) Thereof 1,209 with geography defined and 7 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 
Cited  
Saved (final revised paper)  
No saved metrics found.
Saved (discussion paper)  
No saved metrics found.
Discussed (final revised paper)  
No discussed metrics found.
Discussed (discussion paper)  
No discussed metrics found.
Latest update: 12 Nov 2019
Publications Copernicus
Download
Short summary
This paper presents geochemical data from a suite of glacially eroded igneous rock clasts sampled from Antarctica to estimate both crustal heat production and heat flow for the continental interior. The results indicate that the interior of East Antarctica is underlain by Proterozoic continental lithosphere of average surface heat flow, providing first-order constraints on both geodynamic history and ice-sheet stability.
This paper presents geochemical data from a suite of glacially eroded igneous rock clasts...
Citation