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Principal metalliferous mineral occurrences in the Grampian Highlands. From: Figure 43 in Stephenson, D, and Gould, D. 1995. British regional geology: Grampian Highlands. Fourth edition. Keyworth, Nottingham: British Geological Survey.
|1||Stotfield||G||G1||Naylor et al., 1989|
|2||Littlemill||C||Cp PGM Pn Po||Fletcher and Rice, 1989|
|4||Arthrath||C||Cp PGM Pn Po||Rice, 1975; Gallagher, 1991a|
|5||Kelman Hill||C||PGM Po||Gunn et al., 1990|
|6||Rhynie||E||(As Au Sb)||Rice and Trewin, 1988|
|7||Lecht||B||Mx||Smith, 1985; Nicholson and Anderton, 1989; Smith et al., 1991|
|8||Gairnshiel||D||Bm Ct Fl Mb Sp Wo||Webb et al., 1992|
|9||Abergairn||H||Fl Gl Sp||Dunham, 1952; Gallagher, 1991a|
|10||Coire Loch Kander||A||Bt Gl Sp||Gallagher et al., 1989; Fortey et al., 1991; Fortey et al., 1993|
|13||Duntanlich Ben Eagach Foss||A||Bt Cn Sp Gl||Coats et al., 1981; Fortey and Beddoe-Stephens, 1982; Moles, 1982; Willan and Coleman, 1983|
|14||Glen Lyon||A||Gl Sp||Coats et al., 1984|
|15||Calliachar Burn||H||Ap Cp Gl Go Sp||Mason et al., 1991|
|16||Loch Lyon||A||Bt Cn Gl Sp||Coats et al., 1984|
|17||Tomnadashan||D||Ap Bm Cp Mb St||Pattrick, 1984|
|18||Corriecharmaig||C||Ch||Harrison, 1985; Hawson and Hall, 1987|
|19||Corrie Buie||H||Bm Cp Gl Go Sp||Pattrick, 1984|
|20||Auchtertyre||A||Cp Gl Mb Sp||Fortey and Smith, 1986; Smith et al., 1988; Scott et al., 1988|
|21||Tyndrum||H||Bt Cp Gl Sp Tt Ur||Pattrick et al., 1988; Pattrick et al., 1991|
|22||Cononish||H||Cp Gl Go Sp Te||Parker et al., 1989; Earls et al., 1992|
|23||Lagalochan||D||Ap Cp Gl Go Sp St Te||Harris et al., 1988|
|24||Coille-braghad||A||Po Cp||Wilson and Flett, 1921|
|25||McPhun’s Cairn||A||Cp Gl Sp||Smith et al., 1977; Willan and Hall, 1980|
|26||Kilmartin||H||Cp||Wilson and Flett, 1921|
|27||Meall Mor||A||Cp Gl Sp St||Smith et al., 1978; Mohammed, 1987|
|28||Mulreesh||H||Cp Gl Sp||Wilson and Flett, 1921; Barnett, 1959|
|Mineralogy: Brackets indicate chemical elements, not minerals|
|Key to types of metaliferous mineral occurences|
|Types of metalliferous mineral occurrence|
|G Hosted by Permo-Triassic sedimentary rock|
|F Hosted by Middle Devonian sedimentary rock|
|D Associated with granite and diorite|
|C Associated with basic and ultramafic rocks|
|A Dalradian stratabound|
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