Loch an Daimh Mor Complex

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Journal Article
Published: 03 April 2020
Journal of the Geological Society (2020) 177 (4): 700–717.
... into the tonalite–trondhjemite–granodiorite-dominated crust prior to polyphase metamorphism, representing a significant re-evaluation of the magmatic evolution of the Lewisian Gneiss Complex. Of the other occurrences, two remain ambiguous, but one (Loch an Daimh Mor) has some geochemical affinity with abyssal...
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Simplified geological maps of the ( a ) <span class="search-highlight">Loch</span> Eilean na Craoibhe Moire, ( b ...
Published: 03 April 2020
Fig. 2. Simplified geological maps of the ( a ) Loch Eilean na Craoibhe Moire, ( b ) Drumbeg, ( c ) Loch an Daimh Mor and ( d ) Gnoc Gorm complexes. The location of each complex is shown in Figure 1 . TTG, tonalite–trondhjemite–granodiorite.
Simplified geological map of the Lewisian Gneiss <span class="search-highlight">Complex</span> detailing the loca...
Published: 03 April 2020
Auskaird; BD, Ben Dreavie; BS, Ben Strome; Db, Drumbeg; GC, Gorm Chnoc; GnS, Geodh’ nan Sgadan; LDM, Loch an Daimh Mor; LE, Loch Eilean na Craoibhe Moire; NSB, North Scourie Bay; Sm, Scouriemore.
Journal Article
Published: 01 November 2009
Scottish Journal of Geology (2009) 45 (2): 99–105.
.... They are particularly clear adjacent to Loch Lurgainn; around Achiltibuie in Coigach; on the southern flanks of Little Loch Broom; and further west around Gruinard Bay, Loch Ewe, and on Rubha Mor ( Fig. 2 ). In many cases, these form merely the onshore extent of a well-preserved suite of moraines found across...
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Journal Article
Published: 01 June 2009
Scottish Journal of Geology (2009) 45 (1): 19–41.
... nam Uidh and Clar Loch Cnoc Thormaid. Much of the southwestern limb consists of banded hornblende granulite but patches of apparently unmodified or little modified pyroxene granulite remain, as between Upper Badcall and Loch an Daimh Mor, south of Lower Badcall and around Rudha Gisgil and to the east...
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Journal Article
Published: 01 April 1974
Journal of the Geological Society (1974) 130 (2): 125–150.
.... The 'contact' specimen from the same granite gneiss band, i6, clearly lies on the 2540 m.y. isochron, but 4, from the isoclinally-folded granite gneiss sheet on the Scourie road near Loch an Daimh The Inverian metamorphism and the Lewisian of Lochinver, NW Scotland 141 Mor, may be older. Our interpretation...
Journal Article
Published: 01 January 2008
American Mineralogist (2008) 93 (1): 187–197.
... grain from the margin a syntectonic pyroxenite intrusion in the Lewisian gneiss terrain of northwest Scotland ( Kinny and Friend 1997 ), located at Loch an Daimh Mor (58° 19′54″N, 5°07′57″W). The grain is largely uniform in CL, and is disrupted by CL-dark bands that relate to microstructures associated...
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Book Chapter

C. M. Rice
Series: Geological Society, London, Geology of Series
Published: 01 January 2002
DOI: 10.1144/GOS4P.16
EISBN: 9781862393905
... structural relationship. Smith et al. (1977), Coats et al. (1984a, b, 1987), Pease et al. (1986). Allt an Daimh. Iron sulphides, galena and sphalerite in lower laminated quartzite member of Ben Eagach Schist. Braemar Area* Allt an Loch Stratiform baryte bed (5m thick, 0.8 km length...
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