Structure of the Assynt window, Moine Thrust Zone and relationship of thrusts to alkaline igneous complexes, Caledonian orogeny, NW Scotland
The Moine Thrust Zone forms the Caledonian orogenic thrust front where the Moine Supergroup metamorphic rocks have been thrust westward across the Laurentia plate stable foreland, comprising Archean-Proterozoic granulite and amphibolite facies rocks (Lewisian gneisses), with unconformably overlying...
Prif Awdur: | Searle, MP |
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Fformat: | Journal article |
Iaith: | English |
Cyhoeddwyd: |
Cambridge University Press
2023
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Eitemau Tebyg
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Relationships between the Loch Ailsh and Borralan alkaline intrusions and thrusting in the Moine Thrust zone, southern Assynt culmination, NW Scotland
gan: Searle, MP, et al.
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Structure of the Northern Moine thrust zone, Loch Eriboll, Scottish Caledonides
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The Caledonian Orogeny redefined
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The Caledonian Orogeny redefined
gan: McKerrow, W, et al.
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Reply to Dewey and Ryan Comment on Searle, MP (2021) ‘Tectonic evolution of the Caledonian orogeny in Scotland: a review based on the timing of magmatism, metamorphism and deformation’
gan: Searle, MP
Cyhoeddwyd: (2022)