Geological constraints on the dynamic emplacement of cone-sheets–The Ardnamurchan cone-sheet swarm, NW Scotland
Cone-sheets are a significant constituent of many central volcanoes, where they contribute
to volcano growth by intrusion and through flank eruptions, although the exact emplacement …
to volcano growth by intrusion and through flank eruptions, although the exact emplacement …
Pāhoehoe lava emplacement in Lon Reudle, Mull
SNA Walker, JA Cortés - Scottish Journal of Geology, 2024 - lyellcollection.org
The base of the Mull Lava Sequence, part of the Paleogene British Igneous Province,
contains a variety of volcanic features; for example, small-scale filled lava tubes and toes …
contains a variety of volcanic features; for example, small-scale filled lava tubes and toes …
Emplacement of sub-volcanic cone sheet intrusions
C Magee - 2011 - etheses.bham.ac.uk
Sub-volcanic intrusive networks, of which cone sheets are recognised as a major
constituent, control volcano growth and eruption style. The accepted cone sheet model is …
constituent, control volcano growth and eruption style. The accepted cone sheet model is …
The centre 3 layered gabbro intrusion, Ardnamurchan, NW Scotland
B O'driscoll - Geological Magazine, 2007 - pubs.geoscienceworld.org
Detailed remapping of the Palaeogene Ardnamurchan Centre 3 gabbros, NW Scotland,
suggests that this classic sequence of ring-intrusions forms a composite layered lopolith …
suggests that this classic sequence of ring-intrusions forms a composite layered lopolith …