Transcurrent faults and associated cataclasis in Shetland
- 1 March 1977
- journal article
- Published by Geological Society of London in Journal of the Geological Society
- Vol. 133 (3), 231-247
- https://doi.org/10.1144/gsjgs.133.3.0231
Abstract
No abstract availableKeywords
This publication has 17 references indexed in Scilit:
- Microscopic feather fractures in the faulting processTectonophysics, 1976
- Evidence for post-Hercynian transcurrent movement on the Great Glen Fault in the Moray firthScottish Journal of Geology, 1975
- Interpretation of geophysical observations between the Orkney and Shetland IslandsJournal of the Geological Society, 1975
- Evidence against post-Hercynian transcurrent movement on the Great Glen FaultScottish Journal of Geology, 1975
- The Great Glen Fault in the Shetland AreaNature, 1970
- Deep Sedimentary Basins proved in the Shetland–Hebridean Continental Shelf and MarginNature, 1970
- A geological interpretation of the aeromagnetic maps of the continental shelf around Orkney and ShetlandGeological Journal, 1969
- The metamorphic rocks of the southern part of the Mainland of ShetlandGeological Journal, 1967
- Continuation of the Great Glen Fault beyond the Moray FirthNature, 1961
- ON THE NAPPE STRUCTURE OF NORTH-EAST SHETLANDQuarterly Journal of the Geological Society, 1958