Articles | Volume 35, issue 6
https://doi.org/10.5194/ejm-35-969-2023
https://doi.org/10.5194/ejm-35-969-2023
Research article
 | 
14 Nov 2023
Research article |  | 14 Nov 2023

Symplectite and kelyphite formation during decompression of mafic granulite from Gjelsvikfjella, central Dronning Maud Land, Antarctica

Synnøve Elvevold, Joachim Jacobs, Leif-Erik Rydland Pedersen, Øyvind Sunde, Ane K. Engvik, and Per Inge Myhre

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Short summary
The present study of mafic rocks from Jutulsessen, Gjelsvikfjella, extends the presence of high-pressure rocks in the Maud Belt in Dronning Maud Land, Antarctica. The physical conditions necessary for the development of these rocks were attained during continent–continent collision along the East African–Antarctic Orogen. The new data in this study largely confirm the geodynamic implication outlined by others for the region.