Results of recent geological and geophysical investigations in Moray Firth, Scotland.

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

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