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all geography including DSDP/ODP Sites and Legs
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Europe
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Europe
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soft sediment deformation
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GeoRef Categories
Era and Period
Epoch and Age
Book Series
Date
Availability
The Mesoproterozoic Stac Fada Member, NW Scotland: an impact origin confirmed but refined Available to Purchase
Ice-rafting in lakes in the early Neoproterozoic: dropstones in the Diabaig Formation, Torridon Group, NW Scotland Available to Purchase
Physical and biological functioning in Proterozoic rivers: evidence from the archetypal pre-vegetation alluvium of the Torridon Group, NW Scotland Available to Purchase
Rupture geometries in anisotropic amphibolite recorded by pseudotachylytes in the Gairloch Shear Zone, NW Scotland Available to Purchase
Evidence for pre-Caledonian discontinuities in the Achnashellach Culmination, Moine Thrust Zone: the importance of a pre-thrust template in influencing fold-and-thrust belt development Available to Purchase
The Palaeoproterozoic global carbon cycle: insights from the Loch Maree Group, NW Scotland Available to Purchase
Structure and evolution of the Lewisian Gairloch shear zone: variable movement directions in a strike-slip regime Available to Purchase
Rock-slope failure at Baosbheinn, Wester Ross, NW Scotland: age and interpretation Available to Purchase
Grenville-age pseudotachylite in the Lewisian: laserprobe 40 Ar/ 39 Ar ages from the Gairloch region of Scotland (UK) Available to Purchase
The late Mesoproterozoic–early Neoproterozoic tectonostratigraphic evolution of NW Scotland: the Torridonian revisited Available to Purchase
Multiple fluid migration events along the Moine Thrust Zone, Scotland Available to Purchase
The origin and tectonic significance of Lewisian- and Torridonian-hosted clastic dykes near Gairloch, NW Scotland Available to Purchase
Holocene coastal dune development on the South Erradale peninsula, Wester Ross, Scotland Available to Purchase
Abstract This Memoir presents a detailed account of one of the most critical and interesting parts of the Lewisian complex of NW Scotland; a detached fragment of a supercontinent made up of Laurentia, Siberia and Baltica, which existed at the end of the early Proterozoic period. The Gairloch area, together with neighbouring Loch Maree, is the only part of the mainland Lewisian outcrop where Palaeoproterozoic supracrustal rocks (the Loch Maree Group] and their relationships to the Archaean basement can be studied, and has been the subject of a considerable amount of research, spanning a period of more than forty years. The Loch Maree Group represents an amalgamation of oceanic, trench, and arc assemblages with continental basement, and forms part of a Palaeoproterozoic collisional orogen stretching from Labrador through South Greenland to Scandinavia. The author is Emeritus Professor of Tectonic Geology at Keele University, England, and has studied the structural geology of Precambrian terrains in many parts of the world. He has mapped the area covered by the Memoir in detail, at a scale of 1:10 000, and has an intimate knowledge of the geology, acquired over many years.