Crustal thickening and ductile extension in the NE Greenland Caledonides: a metamorphic record from anatectic pelites

Caledonian orogenesis in NE Greenland resulted from the collision of Laurentia and Baltica during the Ordovician–Silurian. Anatectic pelites within the metasedimentary Smallefjord Sequence record a clockwise P – T path, the result of early crustal thickening at c . 445–440 Ma and subsequent exhumati...

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Bibliographic Details
Published in:Journal of Metamorphic Geology
Main Authors: Jones, K. A., Strachan, R. A.
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2000
Subjects:
Online Access:http://dx.doi.org/10.1046/j.1525-1314.2000.00282.x
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1046%2Fj.1525-1314.2000.00282.x
https://onlinelibrary.wiley.com/doi/pdf/10.1046/j.1525-1314.2000.00282.x