The dolerites of Ardnamurchan
- 7 June 1974
- journal article
- Published by Geological Society of London in Scottish Journal of Geology
- Vol. 10 (1) , 71-89
- https://doi.org/10.1144/sjg10010071
Abstract
Synopsis: Detailed petrochemical work on dolerites from, each of the three centres of Tertiary igneous activity in Ardnamurchan suggests that the (calculated) composition of the initial magmatic liquid giving rise to the Centre 1 dolerites is SiO 2 52.5%, TiO 2 1%, A1 2 O 3 13.5%, total iron 9.5%, MgO 8.5%, CaO 12%, Na 2 O 2% and K 2 O 1%, on a water-free basis. The early dolerites of Ardnamurchan (Centre 1) are relatively richer in SiO 2 , Cu and Ba, and poorer in A1 2 O 3 and Na 2 O than the late dolerites of Centres 2 and 3.Keywords
This publication has 9 references indexed in Scilit:
- The basic intrusive rocks of Caledonian age of the Haddo House and Arnage districts, AberdeenshireScottish Journal of Geology, 1967
- Cryptic layering in the Belhelvie intrusion, AberdeenshireScottish Journal of Geology, 1966
- XII.—The Structure and Form of the Granophyric Quartz-Dolerite Intrusion, Centre II, Ardnamurchan, ArgyllshireTransactions of the Royal Society of Edinburgh, 1966
- The distribution of trace-elements in the Dunite-Syenite Differentiated Series of the Insch Complex, AberdeenshireProceedings of the Geologists' Association, 1963
- Origin of Basalt Magmas: An Experimental Study of Natural and Synthetic Rock SystemsJournal of Petrology, 1962
- The layered ultrabasic rocks of south-west Rhum, Inner HebridesPhilosophical Transactions of the Royal Society of London. B, Biological Sciences, 1961
- The structure and petrology of the hypersthene-gabbro intrusion, Ardnamurchan, ArgyllshireQuarterly Journal of the Geological Society, 1953
- Differentiation of the Palisade diabase, New JerseyGSA Bulletin, 1940
- Cone-sheets and ring-dykes: the dynamical explanationBulletin of Volcanology, 1937