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UK | |
| Preston, R. J., Hole, M. J., & Still, J. (2000). The occurrence of Zr-bearing amphiboles and their relationships with the pyroxenes and biotites in the teschenite and nepheline syenites of a differentiated dolerite boss, Islay, NW Scotland. Mineralogical Magazine, 64(3), 459-468. doi.org/10.1180/002646100549526 Preston, R. J., Hole, M. J., & Still, J. (1999). Exceptional REE-enrichment in apatite during the low pressure fractional crystallisation of alkali olivine basalt Preston, J., Hole, M., Bouch, J., & Still, J. (1998). The occurrence of zirconian aegirine and calcic catapleiite (CaZrSi3O9. 2H2O) within a nepheline syenite, British Tertiary Igneous Province. Scottish Journal of Geology, 34(2), 173-180. doi.org/10.1144/sjg34020173 Hole, M. J., & Morrison, M. A. (1992). The differentiated dolerite boss, Cnoc Rhaonastil, Islay: a natural experiment in the low pressure differentiation of an alkali olivine-basalt magma. Scottish Journal of Geology, 28(1), 55-69. doi.org/10.1144/sjg28010055 an example from the British Tertiary Igneous Province. Earth and Environmental Science Transactions of The Royal Society of Edinburgh, 90(4), 273-285. doi.org/10.1017/S0263593300002637 |
| Cann, J.R. (1965) The metamorphism of amygdales at 'S Airde Beinn, Northern Mull. Mineralogical Magazine, vol. 34, n° 268, 92-106. |
| Upton, B. G. J., Aspen, P., Rex, D. C., Melcher, F., & Kinny, P. (1998). Lower crustal and possible shallow mantle samples from beneath the Hebrides: evidence from a xenolithic dyke at Gribun, western Mull. Journal of the Geological Society, 155(5), 813-828. doi.org/10.1144/gsjgs.155.5.0813 B.G.J. Upton et al. , Journal of the Geological Society, 1998, V 155, N° 5, pp 813-828. |
- Wanlock Dod-Whytes Cleuch
| Day, Harry (1999) BMS Database, British Micromount Society. |
| S.Rust Collection |
| www.alexstrekeisen.it (2014) http://www.alexstrekeisen.it/english/pluto/lugarite.php |
| Neall, T. (2005) Cassedanneite from Lady Anne Hopetoun Shaft, Leadhills, Scotland. Uk Journal of Mines and Minerals 26, 29-30 |