Metamorphic history of high‐pressure granulites in Payer Land, Greenland Caledonides

Abstract A high‐ P granulite facies gneiss complex occurs in north‐west Payer Land (74°28′−74°47′N) in the central part of the East Greenland Caledonian (Ordovician–Devonian) orogen. High‐ P metamorphism of the Payer Land gneiss complex resulted in formation of the assemblages Grt + Cpx + Amp + Qtz...

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Bibliographic Details
Published in:Journal of Metamorphic Geology
Main Authors: Elvevold, S., Thrane, K., Gilotti, J. A.
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2002
Subjects:
Online Access:http://dx.doi.org/10.1046/j.1525-1314.2003.00419.x
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