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...
Published in: | Journal of Metamorphic Geology |
---|---|
Main Authors: | , , , |
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 |