Edifice and substrata deformation induced by intrusive complexes and gravitational loading in the Mull volcano (Scotland)

Author:

Mathieu Lucie,Vries Benjamin van Wyk de

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology

Reference32 articles.

1. Anderson DL, Natland JH (2005) A brief history of the plume hypothesis and its competitors; concept and controversy. Geol Soc Am Special Paper 388:119–145

2. Bailey EB, Clough CT, Wright WB, Richey JE, Wilson GV (1924) Tertiary and post-tertiary geology of Mull, Loch Aline and Oban. Mem Geol Surv Great Brit 44:172–184

3. Bailey EB (1962) Early tertiary fold movements in Mull. Geol Mag 99:478–479

4. Boudon G, Semet MP, Vincent PM (1992) Les éruptions à écroulement de flanc sur le volcan de la Grande Découverte (la Soufriére) de Guadeloupe: implications sur le risque volcanique. Bull Soc Géol Fr 163:159–167

5. Chambers LM, Pringle MS (2001) Age and duration of activity at the Isle of Mull tertiary igneous centre, Scotland, and confirmation of the existence of subchrons during anomaly 26r. EPSL 193:333–345

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