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GeoRef Categories
Era and Period
Epoch and Age
Book Series
Date
Availability
Ben Loyal Intrusion
The influence of country rock structural architecture during pluton emplacement: the Loch Loyal syenites, Scotland Available to Purchase
The structure and petrology of the Cnoc nan Cuilean Intrusion, Loch Loyal Syenite Complex, NW Scotland Available to Purchase
Syn-orogenic alkaline magmatism and its relationship to the Moine Thrust Zone and the thermal state of the Lithosphere in NW Scotland Available to Purchase
Geology of the Loch Loyal Syenite Complex based on King ( 1942 ), Robertson... Available to Purchase
Simplified geological map of the Northern Highlands, showing the main struc... Available to Purchase
Regional geology of north Sutherland (modified from British Geological Sur... Available to Purchase
Summary of geochronology data across northernmost Scotland. ( a ) All recen... Free
Discussion on the influence of country rock structural architecture during pluton emplacement: the Loch Loyal syenites, Scotland Available to Purchase
Timing of regional deformation and development of the Moine Thrust Zone in the Scottish Caledonides: constraints from the U–Pb geochronology of alkaline intrusions Available to Purchase
Structural, petrological, and tectonic constraints on the Loch Borralan and Loch Ailsh alkaline intrusions, Moine thrust zone, northwestern Scotland Open Access
Structure of the Assynt window, Moine Thrust Zone and relationship of thrusts to alkaline igneous complexes, Caledonian orogeny, NW Scotland Open Access
The geology and structural evolution of a Caledonian fold and ductile thrust zone, Kyle of Tongue region, Sutherland, northern Scotland Available to Purchase
Trace element minerals from carbonatite-related fluids, The Aird, Scotland Available to Purchase
Mineralogical Association of Canada Free
Relationships between the Loch Ailsh and Borralan alkaline intrusions and thrusting in the Moine Thrust zone, southern Assynt culmination, NW Scotland Available to Purchase
Abstract The Moine Thrust zone of NW Scotland marks the Caledonian orogenic front and in the Assynt region consists of several west-vergent major thrust sheets (Moine, Ben More, Glencoul and Sole Thrust sheets) that place allochthonous rocks onto the Lewisian basement and Torridon Group cover in the west. Here we present two new balanced and restored sections across the Moine Thrust zone in the region of the Loch Ailsh and Loch Borralan alkali intrusions. Syenites and alkaline pyroxenites intrude up to Durness Group carbonates. Syenites are interpreted as cut by the Moine and Ben More Thrusts and therefore their intrusion age ( c . 430 Ma) provides a maximum age constraint on cessation of motion along the Moine Thrust. We review and discuss several controversies, notably: (1) relationships between folding in the Ben More Thrust sheet (Sgonnan Mor folds) and fabric development associated with intrusion of the Loch Ailsh pluton and initiation of the Moine and Ben More Thrusts; (2) structural relationships around the Borralan intrusion, particularly the nature of its basal and lateral margins (intrusive or thrust-ramp); (3) the structural relationships of the Cam Loch and Benn Fhuarain klippen; and (4) the timing of motion of all thrust sheets in the southern Assynt culmination.