The Ben Nevis Intrusive Ring Tuff, Scotland: re-interpretation of the ‘Flinty Crush Rock’ as part of an ignimbrite conduit in the roots of an ancient caldera-Reference-Cited by-同舟云学术

The Ben Nevis Intrusive Ring Tuff, Scotland: re-interpretation of the ‘Flinty Crush Rock’ as part of an ignimbrite conduit in the roots of an ancient caldera

Published:1997-11 Issue:2 Volume:33 Page:149-155
ISSN:0036-9276
Container-title:Scottish Journal of Geology
language:en
Short-container-title:Scottish Journal of Geology

Author:

Burt R. M.,Brown P. E.

Publisher

Geological Society of London

Subject

Geology

Reference29 articles.

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2. The Marginal intrusions of Ben Nevis; Coille Lèanachain Complex; and the Ben Nevis Dyke swarm;ANDERSON;Transactions of the Geological Society Glasgow,1935

3. BAILEY E. B. 1960. The geology of Ben Nevis and Glen Coe and the surrounding country. Memoirs of the Geological Survey of Great Britain, 53 (2nd edition).

4. BAILEY E. B. MAUFE H. B. 1916. The geology of Ben Nevis and Glen Coe and the surrounding country. Memoirs of the Geological Survey of Great Britain, 53 (1st edition).

5. BURT R. M. 1994. The geology of Ben Nevis, Southwest Highlands, Scotland. University of St. Andrews, Ph.D. thesis (unpublished).

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1. Digital Mapping and Three-Dimensional Model Building of the Ben Nevis Igneous Complex, Southwest Highlands, Scotland: New Insights into the Emplacement and Preservation of Postorogenic Magmatism;The Journal of Geology;2017-11

2. Geology and complex collapse mechanisms of the 3.72 Ma Hannegan caldera, North Cascades, Washington, USA;Geological Society of America Bulletin;2007-03-01