Retrogression by deep infiltration of meteoric fluids into thrust zones during late‐orogenic rapid unroofing

Hypersaline (Na–Ca–Cl) fluids are associated with late‐stage quartz veining and retrogression of garnet, kyanite and other high P–T phases in the vicinity of thrusts and major lithological boundaries in the Scandian nappes of the Troms‐Ofoten region, northern Norway. They record early Devonian fluid...

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Bibliographic Details
Published in:Journal of Metamorphic Geology
Main Authors: Barker, Bennett, Boyce, Fallick
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2000
Subjects:
Online Access:http://dx.doi.org/10.1046/j.1525-1314.2000.00257.x
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1046%2Fj.1525-1314.2000.00257.x
https://onlinelibrary.wiley.com/doi/pdf/10.1046/j.1525-1314.2000.00257.x