Metamorphism of the Scourian Complex, NW Scotland
Author:
Publisher
Wiley
Subject
Geochemistry and Petrology,Geology
Link
http://onlinelibrary.wiley.com/wol1/doi/10.1111/j.1525-1314.1983.tb00270.x/fullpdf
Reference79 articles.
1. A. C. Barnicoat , 1982 . Thermal history of parts of the Lewisian gneiss complex, NW Scotland. Unpubl. Ph.D. thesis, Univ. of Edinburgh.
2. High-temperature pyroxenes from an ironstone at Scourie, Sutherland
3. 2,390 Myr Rb–Sr whole-rock for the Scourie dykes of north-west Scotland
4. Lead isotope measurements from the oldest recognised Lewisian gneisses of north-west Scotland
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1. Origin of ultramafic–mafic bodies on the Isles of Lewis and Harris (Scotland, UK): Constraints on the Archean–Paleoproterozoic evolution of the Lewisian Gneiss Complex, North Atlantic Craton;Precambrian Research;2022-02
2. Seeing through metamorphic overprints in Archean granulites: combined high resolution thermometry and phase equilibrium modeling of the Lewisian Complex, Scotland;American Mineralogist;2021-10-01
3. Origin(s) and geodynamic significance of Archean ultramafic–mafic bodies in the mainland Lewisian Gneiss Complex, North Atlantic Craton;Journal of the Geological Society;2020-03-05
4. New constraints on granulite facies metamorphism and melt production in the Lewisian Complex, northwest Scotland;Journal of Metamorphic Geology;2018-04-22
5. Subduction or sagduction? Ambiguity in constraining the origin of ultramafic–mafic bodies in the Archean crust of NW Scotland;Precambrian Research;2016-09
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