Articles | Volume 35, issue 4
https://doi.org/10.5194/ejm-35-479-2023
https://doi.org/10.5194/ejm-35-479-2023
Research article
 | 
17 Jul 2023
Research article |  | 17 Jul 2023

Detrital garnet petrology challenges Paleoproterozoic ultrahigh-pressure metamorphism in western Greenland

Jan Schönig, Carsten Benner, Guido Meinhold, Hilmar von Eynatten, and N. Keno Lünsdorf

Viewed

Total article views: 868 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
637 212 19 868 57 14 18
  • HTML: 637
  • PDF: 212
  • XML: 19
  • Total: 868
  • Supplement: 57
  • BibTeX: 14
  • EndNote: 18
Views and downloads (calculated since 17 Jul 2023)
Cumulative views and downloads (calculated since 17 Jul 2023)

Viewed (geographical distribution)

Total article views: 848 (including HTML, PDF, and XML) Thereof 848 with geography defined and 0 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 13 Dec 2024
Download
Short summary
When and how modern-style plate tectonics initiated is a matter of debate. Although the earliest unequivocal evidence for ultrahigh-pressure metamorphism is Neoproterozoic, similar processes have been proposed for Paleoproterozoic rocks of western Greenland. We intensely screened the area by studying detrital heavy minerals, garnet chemistry, and mineral inclusion assemblages in garnet. Our results raise considerable doubts on the existence of Paleoproterozoic ultrahigh-pressure rocks.