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Strathmore Basin

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Journal Article
Published: 01 May 2000
Journal of Micropalaeontology (2000) 19 (1): 45–59.
...H. A. ARMSTRONG Abstract Mid-Ordovician limestone clasts in the Lower Old Red Sandstone conglomerates of the Lanark and Strathmore basins of the Midland Valley, Scotland, were derived from a cryptic carbonate platform, now hidden beneath the Southern Uplands Allochthon. These have yielded 17 multi...
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Journal Article
Published: 01 June 2005
Bulletin of Canadian Petroleum Geology (2005) 53 (2): 154–164.
... appearance of M. striatus , a species that to date has not been observed in Canada. Sweet et al. (1989) , in a study of the Brackett Coal Basin in the Northwest Territories, established a series of informal zones. The studied Strathmore well section would be included in their Aquilapollenites...
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Series: Geological Society, London, Special Publications
Published: 01 January 2000
DOI: 10.1144/GSL.SP.2000.180.01.24
EISBN: 9781862394285
... Abstract Conodont-bearing limestone clasts in Lower Old Red Sandstone conglomerates in the Lanark and Strathmore basins and the Pentland Hills Inlier, Midland Valley, Scotland, indicate a source in a cryptic arc terrane with a mid-Ordovician (P. serra – P. anserinus Biozone) limestone cover...
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Journal Article
Published: 20 August 2012
Canadian Journal of Earth Sciences (2012) 49 (9): 1053–1086.
...David A. Eberth; Dennis R. Braman Abstract The Upper Cretaceous paralic to nonmarine Horseshoe Canyon Formation (HCFm) of southern Alberta is divided into seven mappable members: Strathmore, Drumheller, Horsethief, Morrin, Tolman, Carbon, and Whitemud (bottom to top). This subdivision, based...
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Journal Article
Published: 01 June 1994
Journal of the Geological Society (1994) 151 (3): 425–438.
... with a thinner succession in Angus and Perthshire thinning again to the SW where the Lower ORS is just over 1 km thick on Arran, the Kintyre peninsula, and the Balmaha area. Recent research suggests that it is incorrect to view all the Strathmore Lower ORS as the fill to a single basin, as previously attempted...
Journal Article
Published: 23 September 2015
Scottish Journal of Geology (2015) 51 (2): 165–176.
.... The conglomerate–sandstone sequence beneath was also deposited in alluvial fans that accumulated in a strike-slip, extensional basin in which units of conglomerate become progressively younger to the SW. Immediately NW of the Gualann Fault, in the Queen Elizabeth Forest, sub-horizontal red sandstones and breccias...
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Journal Article
Published: 01 February 1995
Journal of the Geological Society (1995) 152 (1): 196.
... (Kincardineshire) and 1.3% for the Strathmore Group (Perthshire). They conclude that 'the Stonehaven Group reflectivity values are considerably lower than expected under the 9 km of sediments aggregated for the Lower ORS of Kincardineshire and demonstrate a maximum burial of 3 to 5 km’. The ORS correlates...
Journal Article
Published: 01 September 2008
Journal of the Geological Society (2008) 165 (5): 915–921.
... undetected movement on a proto-Highland Boundary Fault at a time when major orogen-parallel, sinistral strike-slip was thought to have taken place ( Dewey & Strachan 2003 ), with the fault being buried subsequently under the Lower Old Red Sandstone fill of the Strathmore Basin. However, this poses...
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Journal Article
Published: 01 April 2005
Scottish Journal of Geology (2005) 41 (1): 3–11.
... intergranular flow dominates. The most productive bedrock aquifers are the Permian sandstones and breccia in SW Scotland and the Devonian sandstones in Fife, Strathmore and Morayshire. Alluvium and fluvio-glacial sands and gravels can also form important aquifers and provide some of Scotland’s most highly...
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Journal Article
Published: 01 April 2006
Scottish Journal of Geology (2006) 42 (1): 1–19.
...-Carboniferous sandstones in the giant Clair field located on the Rona Ridge ( Coney et al. 1993 ), through Middle and Upper Jurassic sandstones in the Solan and Strathmore fields ( Herries et al. 1999 ), to the main reservoir play, the late Paleocene deep-water sandstones of the Foinaven Sub-basin fields...
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Series: Geological Society, London, Special Publications
Published: 01 January 2001
DOI: 10.1144/GSL.SP.2001.188.01.03
EISBN: 9781862394360
... systems south of Ireland and the UK. The main oil discoveries in the West of Shetlands are located in the Faroe-Shetland Basin, comprising the Clair, Foinaven and Schiehallion/Loyal oil fields and the Suilven oil discovery ( Fig. 1 ), and the West Shetland Basin, comprising the Solan/Strathmore and 204...
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Series: Geological Society, London, Special Publications
Published: 01 January 2002
DOI: 10.1144/GSL.SP.2002.196.01.21
EISBN: 9781862394445
... in the Solan Basin, small oil accumulations (Solan and Strathmore) totalling 60MMB occur in Upper Jurassic and Triassic truncation traps. The non-biodegraded oil was sourced from a limited kichen area, the East Solan Basin, where the Upper Jurassic source rocks are at early oil maturity ( Herries et al. 1999...
Series: Geological Society, London, Special Publications
Published: 01 January 2000
DOI: 10.1144/GSL.SP.2000.180.01.22
EISBN: 9781862394285
... centres aligned along a lineament of Caledonian trend and probably on the site of an older, Ordovician–Silurian magmatic arc (Bluck 1983 , 1984 ). This Ayr–Ochil–Sidlaw volcanic axis formed a topographic high in the Devonian Midland Valley and separated the Strathmore basin to the north from the Lanark...
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Journal Article
Published: 08 November 2019
Journal of the Geological Society (2019) jgs2019-063.
... the basement of the northern MVB ( Browne et al. 2002 ). In the northern MVB, the LORS succession is subdivided into the Stonehaven, Dunnottar–Crawton, Arbuthnott–Garvock and Strathmore groups ( Figs 2 and 3 ). The oldest of the groups, the Stonehaven Group, is confined to the NE of the basin ( Fig. 2...
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Series: Geological Society, London, Petroleum Geology Conference series
Published: 01 January 2005
DOI: 10.1144/0061247
EISBN: 9781862394124
...-Carboniferous sandstones in the giant Clair field ( Fig. 5a ) on the Rona Ridge, through Middle and Upper Jurassic sandstones in the Solan and Strathmore fields to the main reservoir play, the late Paleocene deepwater sandstones of the Foinaven sub-basin fields (Foinaven, Schiehallion, Loyal and Suilven) ( Fig...
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Journal Article
Published: 24 June 2013
Journal of the Geological Society (2013) 170 (4): 641–655.
... to comprise part of a volcanic edifice that formed the southern edge of a narrow NE–SW-trending sub-basin (the Strathmore Basin) within the Midland Valley ( Bluck 1984 , 2000 ). A sample of andesite from the Ochil Volcanic Formation yielded an Rb–Sr age of 416.1 ± 6.1 Ma, although this date is not considered...
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Journal Article
Published: 22 January 2015
Journal of the Geological Society (2015) 172 (2): 213–217.
...Adrian J. Hartley; Sophie Leleu Abstract The relationship between movement on the Highland Boundary Fault and deposition of the Lower Old Red Sandstone in the Midland Valley Basin of Scotland is controversial. Most models favour mid-Silurian to early Devonian sinistral movement on the Highland...
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Journal Article
Published: 21 August 2019
Journal of the Geological Society (2019) 176 (6): 1120–1135.
..., Faeroe–Shetland Basin; HB, Hatton Bank; HP, Hebridian Platform; GH, Grampian High; SP, Shetland Platform; SMB, Strathmore Basin; AM, Armorican Massif; GGF, Great Glen Fault. Inset indicates study area ( b ) Regional map showing location of Corrib gas field. Colours of the targeted wells in the Slyne...
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Journal Article
Published: 01 January 1977
Journal of the Geological Society (1977) 133 (1): 37–50.
...P. TURNER Abstract A palaeomagnetic survey has been made of fluviatile red beds and lacustrine flagstones in the Orcadian Basin. The results from five facies are all different in important respects and this suggests that the palaeomagnetic history is strongly influenced by short-term and long-term...
Series: Geological Society, London, Special Publications
Published: 01 January 2002
DOI: 10.1144/GSL.SP.2002.197.01.04
EISBN: 9781862394452
... with the location of the Strathmore Field. Adapted from Lamers and Carmichael (1999) . The reservoir sandstones in the Foinaven Sub-basin are of Late Paleocene (Thanetian) age, and are deepwater in origin, deposited within or related to channelized submarine slope systems ( Cooper et al. 1999 ; Leach et...
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