Solid Earth
Solid Earth
SE
Articles | Volume 9, issue 3
Articles | Volume 9, issue 3
https://doi.org/10.5194/se-9-797-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/se-9-797-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
Articles | Volume 9, issue 3
Research article
 | 
19 Jun 2018
Research article |  | 19 Jun 2018

Ca-rich garnets and associated symplectites in mafic peraluminous granulites from the Gföhl Nappe System, Austria

Konstantin Petrakakis, Nathalie Schuster-Bourgin, Gerlinde Habler, and Rainer Abart

Viewed

Total article views: 3,379 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
1,943 1,306 130 3,379 386 133 121
  • HTML: 1,943
  • PDF: 1,306
  • XML: 130
  • Total: 3,379
  • Supplement: 386
  • BibTeX: 133
  • EndNote: 121
Views and downloads (calculated since 12 Mar 2018)
Cumulative views and downloads (calculated since 12 Mar 2018)

Viewed (geographical distribution)

Total article views: 3,379 (including HTML, PDF, and XML) Thereof 3,003 with geography defined and 376 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Discussed (final revised paper)

Latest update: 29 Jun 2024
Download
Short summary
Aluminum-rich granulites from Austria contain large garnets with kyanite inclusions. Garnets are built up from compositionally different types. They are replaced partially by various symplectites. Thermodynamic analysis points to metasomatic alteration and rock decompression due to tectonic transport at high temperatures from deep to middle crustal levels. The various symplectites were formed after decompression during cooling within a short time interval of less than 500 years.
Read more