Laccolithic, as opposed to cauldron subsidence, emplacement of the Eastern Mourne pluton, N. Ireland: evidence from anisotropy of magnetic susceptibility

Author:

Stevenson Carl T.E.,Owens William H.,Hutton Donald H.W.,Hood David N.,Meighan Ian G.

Publisher

Geological Society of London

Subject

Geology

Reference80 articles.

1. Akiman, O. , 1971. The petrology and geochemistry of the Tertiary dyke swarm associated with the Mourne Mountains granites, N. Ireland. PhD Thesis. University of Durham, Durham.

2. Anderson, T.B. & Cameron, T.D.J. 1979. A structural profile of Caledonian deformation in Down. In: Harris, A.L., Holland, C.H. & Leake, B.E. (eds) The Caledonides of the British Isles — Reviewed. Geological Society, London, Special Publications, 8, 262–267.

3. Bailey, E.B. , Clough, C.T., Wright, W.B., Richey, J.E. & Wilson, G.V. 1924. Tertiary and Post-Tertiary Geology of Mull, Loch Aline, and Oban. Memoirs of the Geological Survey.Scotland: Edinburgh, HMSO.

4. Bell, B.R. & Emeleus, C.H. 1988. A review of silicic pyroclastic rocks of the British Tertiary Volcanic Province. In: Morton, A.C. & Parson, L.M. (eds) Early Tertiary Volcanism and the Opening of the NE Atlantic. Geological Society, London, Special Publications, 39, 365–379.

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