Articles | Volume 9, issue 3
https://doi.org/10.5194/se-9-797-2018
https://doi.org/10.5194/se-9-797-2018
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

Download

Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
Printer-friendly Version - Printer-friendly version Supplement - Supplement

Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Konstantin Petrakakis on behalf of the Authors (25 Apr 2018)  Author's response   Manuscript 
ED: Publish subject to minor revisions (review by editor) (02 May 2018) by Federico Rossetti
AR by Konstantin Petrakakis on behalf of the Authors (17 May 2018)  Author's response   Manuscript 
ED: Publish as is (18 May 2018) by Federico Rossetti
ED: Publish as is (18 May 2018) by Federico Rossetti (Executive editor)
AR by Konstantin Petrakakis on behalf of the Authors (22 May 2018)
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.