Articles | Volume 10, issue 1
https://doi.org/10.5194/se-10-357-2019
https://doi.org/10.5194/se-10-357-2019
Peer-reviewed comment
 | 
27 Feb 2019
Peer-reviewed comment |  | 27 Feb 2019

Comment on “Channel flow, tectonic overpressure, and exhumation of high-pressure rocks in the Greater Himalayas” by Marques et al. (2018)

John P. Platt

Viewed

Total article views: 2,960 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
1,944 908 108 2,960 112 105
  • HTML: 1,944
  • PDF: 908
  • XML: 108
  • Total: 2,960
  • BibTeX: 112
  • EndNote: 105
Views and downloads (calculated since 26 Sep 2018)
Cumulative views and downloads (calculated since 26 Sep 2018)

Viewed (geographical distribution)

Total article views: 2,960 (including HTML, PDF, and XML) Thereof 2,470 with geography defined and 490 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Discussed (final revised paper)

Discussed (preprint)

Latest update: 22 Nov 2024
Short summary
The channel flow model proposed by Marques et al (2018) for the Himalayas has a geometry that would not generate any excess pressure. The excess pressure calculated by the authors, based on a different and highly improbable geometry, is so high that the overlying rocks would not be able to contain it: they would bend or break in such a way as to relieve the pressure. The conclusions drawn by the authors are therefore unwarranted and misleading.