1-4 OF 4 RESULTS FOR

Tarves Scotland

Results shown limited to content with bounding coordinates.
Follow your search
Access your saved searches in your account

Would you like to receive an alert when new items match your search?
Close Modal
Sort by
Journal Article
Published: 16 September 2021
Journal of the Geological Society (2022) 179 (1): jgs2021-040.
...David R.M. Pattison; Shantal A. Goldsmith Abstract The metamorphism of the Buchan block in northeast Scotland, and its relation to the Barrovian domain to its west, have been reassessed from consideration of mineral assemblages, microstructures, phase equilibrium modelling and monazite U–Pb...
FIGURES
First thumbnail for: Metamorphism of the Buchan type-area, NE <span cla...
Second thumbnail for: Metamorphism of the Buchan type-area, NE <span cla...
Third thumbnail for: Metamorphism of the Buchan type-area, NE <span cla...
Journal Article
Published: 01 December 1999
Journal of the Geological Society (1999) 156 (6): 1163–1173.
... 1999 Geological Society of London Scotland Neoproterozoic Caledonides rift basins unconformity References British Geological Survey 1996a. Foyers. Scotland Sheet 73E. Solid Geology. 1:50 000. British Geological Survey. Keyworth, Nottingham. British 1996&. Glenlivet...
Journal Article
Published: 03 May 2007
Canadian Journal of Earth Sciences (2007) 44 (3): 413–431.
... in the world across the Ordovician–Silurian boundary ( Barnes 1988 ), serving as an alternative boundary stratotype, in a shallow-shelf setting, to the graptolitic, deeper water stratotype at Dob’s Linn, Scotland ( Underwood et al. 1997 ). Minor patch reef complexes are present within the Anticosti succession...
FIGURES
First thumbnail for: Tempestite frequency curves: a key to Late Ordovic...
Second thumbnail for: Tempestite frequency curves: a key to Late Ordovic...
Third thumbnail for: Tempestite frequency curves: a key to Late Ordovic...
Journal Article
Published: 01 March 1994
Bulletin of Canadian Petroleum Geology (1994) 42 (1): 26–54.
... the sandstone. It contains tarved silty wave ripples, parallel lamination and rare burrows. This mudstone is erosively over- lain by a 1.5 m thick, upward-fining sandstone unit, exhibiting decimetre scale, planar-tabular c oss bedding, mud-draped SEDIMENTOLOG Y AND HIGH RESOLUTION SEQUENCE ANALYSIS; BEARPA W...