dc.contributor.author | Bacon, M. | |
dc.contributor.author | Chesher, J. | |
dc.date.accessioned | 2020-08-26T13:14:14Z | |
dc.date.available | 2020-08-26T13:14:14Z | |
dc.date.issued | 1975 | |
dc.identifier.uri | https://hdl.handle.net/11250/2674999 | |
dc.description.abstract | Geophysical, shallow drilling and sea-bed sampling investigations have shown that the main sedimentary basin of the Moray Firth is separated by an ENE-trending, horst-like uplift zone from a secondary basin to the south. Mesozoic sequences are broadly conformable and are dissected by a radiate fault pattern; faulting was most active in pre-Mid Jurassic times. Contrary to previous suggestions, the pattern of outcrop preludes any Mesozoic of Tertiary strike-slip movement on the Great Glen Fault. | |
dc.language.iso | eng | |
dc.relation.ispartofseries | NGU (316) | |
dc.rights | Navngivelse 4.0 Internasjonal | |
dc.rights.uri | http://creativecommons.org/licenses/by/4.0/deed.no | |
dc.subject | GEOFYSIKK | |
dc.subject | BERGGRUNNSGEOLOGI | |
dc.subject | BORING | |
dc.title | Results of recent geological and geophysical investigations in Moray Firth, Scotland. | |
dc.type | Journal article | |
dc.description.localcode | 35894 | |
dc.source.pagenumber | 99-104 | |