Articles | Volume 32, issue 1
https://doi.org/10.5194/ejm-32-167-2020
https://doi.org/10.5194/ejm-32-167-2020
Letter
 | 
30 Jan 2020
Letter |  | 30 Jan 2020

Comment on “Water decreases displacive phase transition temperature in alkali feldspar” by Liu et al. (2018)

Herbert Kroll and Peter Schmid-Beurmann

Viewed

Total article views: 1,386 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
1,062 285 39 1,386 27 34
  • HTML: 1,062
  • PDF: 285
  • XML: 39
  • Total: 1,386
  • BibTeX: 27
  • EndNote: 34
Views and downloads (calculated since 30 Jan 2020)
Cumulative views and downloads (calculated since 30 Jan 2020)

Viewed (geographical distribution)

Total article views: 1,283 (including HTML, PDF, and XML) Thereof 1,229 with geography defined and 54 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 
Latest update: 11 Dec 2024
Short summary
Feldspars are the most abundant minerals in the Earth's crust. Their structural behaviour is complicated because order/disorder reactions, phase transitions, and unmixing processes interact. Liu et al. (2018) claim that the water content in the nominally dry feldspars has a profound influence on the transformation behaviour. Their arguments, however, are not sound. We point to a number of errors and omissions.