The Lundy Complex: Its petrology and tectonics
- 1 September 1941
- journal article
- Published by Geological Society of London in Quarterly Journal of the Geological Society
- Vol. 97 (1-4), 39-77
- https://doi.org/10.1144/gsl.jgs.1941.097.01-04.03
Abstract
The Lundy igneous complex projects through the Palaeozoic floor of the Bristol Channel at a point 24 miles due west of Ilfracombe, North-West Devonshire. Its subaerial part lies about the intersection of parallel 51° 11′ N., and meridian 4° 40′ W.Keywords
This publication has 6 references indexed in Scilit:
- The Heavy Mineral Correlation Of Igneous RocksGeological Magazine, 1931
- A Recording Micrometer for Geometrical Rock AnalysisThe Journal of Geology, 1916
- IV.—Pleochroic HalosGeological Magazine, 1910
- On the Morte Slates, and Associated Beds, in North Devon and West Somerset.--Part IQuarterly Journal of the Geological Society, 1896
- On the Occurrence of Topazes in Lundy IslandGeological Magazine, 1870
- On the circumstances and phænomena presented by the Granite of Lundy Island, and of Hestercombe in the Quantock Hills, compared with those which characterise the Granites of Devon and Cornwall.Quarterly Journal of the Geological Society, 1846