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Glenshirra Group

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Journal Article
Published: 01 November 2004
Scottish Journal of Geology (2004) 40 (2): 159–174.
... Pebbly Psammite Formations (hitherto included within the Glenshirra Subgroup at the base of the Neoproterozoic Grampian Group) represent a continuum of alluvial fan to shallow water sediments, deposited in a SE thinning fan-delta clastic wedge. These sediments, derived from an uplifted granitoid...
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First thumbnail for: Sedimentology and stratigraphic affinities of Neop...
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Concordia plans for the Glenshirra Group samples: (a) ID-TIMS data for sample LTF99-1; (b) LA-MC-ICP-MS data for sample LTF99-1; (c) ID-TIMS data for sample LTF99-13 – the boxed area is shown in greater detail in (d); (d) detail of ID-TIMS data between 1450 and 1500 Ma; (e) LA-MC-ICP-MS data for LTF99-13 – data for rim analyses are shown by filled ellipses, those for core analyses by unfilled ellipses; (f) Terra–Wasserburg Concordia plot for zircons from the heavy mineral band, sample LTF99-2 analysed by LA-MC-ICP-MS.
Published: 01 November 2013
Fig. 4. Concordia plans for the Glenshirra Group samples: ( a ) ID-TIMS data for sample LTF99-1; ( b ) LA-MC-ICP-MS data for sample LTF99-1; ( c ) ID-TIMS data for sample LTF99-13 – the boxed area is shown in greater detail in (d); ( d ) detail of ID-TIMS data between 1450 and 1500 Ma; ( e ) LA
Journal Article
Published: 01 November 2013
Scottish Journal of Geology (2013) 49 (2): 81–92.
...Fig. 4. Concordia plans for the Glenshirra Group samples: ( a ) ID-TIMS data for sample LTF99-1; ( b ) LA-MC-ICP-MS data for sample LTF99-1; ( c ) ID-TIMS data for sample LTF99-13 – the boxed area is shown in greater detail in (d); ( d ) detail of ID-TIMS data between 1450 and 1500 Ma; ( e ) LA...
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First thumbnail for: Basement palaeogeography of late Neoproterozoic Sc...
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Representative sandstones of the (meta)sedimentary units south of the Great Glen Fault that are dominated by 1.8–1.6 Ga detrital zircons: (a) Loch Laggan Formation (Grampian Group), Loch Laggan; (b, c) Glenshirra Group, Loch Tarff; (d) Dun Gallain Formation (upper Colonsay Group), Colonsay; (e) Oronsay Formation (lower Colonsay Group), Oronsay. (f) Migmatitic paragneiss of the Badenoch Group, Kincraig.
Published: 13 September 2024
Fig. 6. Representative sandstones of the (meta)sedimentary units south of the Great Glen Fault that are dominated by 1.8–1.6 Ga detrital zircons: ( a ) Loch Laggan Formation (Grampian Group), Loch Laggan; ( b , c ) Glenshirra Group, Loch Tarff; ( d ) Dun Gallain Formation (upper Colonsay Group
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Photographs of debris-flow metaconglomerate from the Loch Tarff area [NH 4185 1130], Glen Buck Pebbly Psammite Formation, Glenshirra Group. Note the matrix-supported nature of the clasts, indicative of en masse flow.
Published: 01 November 2013
Fig. 2. Photographs of debris-flow metaconglomerate from the Loch Tarff area [NH 4185 1130], Glen Buck Pebbly Psammite Formation, Glenshirra Group. Note the matrix-supported nature of the clasts, indicative of en masse flow.
Series: Geological Society, London, Geology of Series
Published: 20 August 2024
DOI: 10.1144/GOS5-2022-12
EISBN: 9781786206893
... Fig. 5.7. Sedimentary features of the Glenshirra and Grampian groups. ( a )–( c ) Glenshirra Group rocks interpreted as alluvial fan-braided fluvial deposits: ( a ) arkosic pebbly psammite with well-rounded quartz-feldspathic (syenitic) cobbles (highlighted by thin yellow outlines) and ( b...
Journal Article
Published: 05 October 2014
Scottish Journal of Geology (2014) 50 (2): 143–158.
... correlation of the Iona Group with the Colonsay Group and the Glenshirra Subgroup of the Dalradian Grampian Group, although correlation with parts of the Torridonian cannot be excluded. Supplementary material: Full analytical results areavailable at http://www.geolsoc.org.uk/SUP18768 . * (e...
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First thumbnail for: Sedimentary provenance, age and possible correlati...
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Journal Article
Published: 01 February 1989
Journal of the Geological Society (1989) 146 (1): 85–96.
.... The possibility that the Grampian Group was unconformable on the structurally underly-ing Central Highland Division and Glenshirra Succession is currently unresolved. 16 2 1988 18 7 1988 © Geological Society of London 1989 1989 Geological Society of London Geological Society of London...
Journal Article
Published: 22 February 2023
Journal of the Geological Society (2023) 180 (2): jgs2022-134.
...://www.lyellcollection.org/topic/collections/the-caledonian-wilson-cycle In summary, the Glenshirra–Grampian–Appin groups are devoid of the typical lithological features that characterize the infill of continental rift basins. By contrast, starting with the early Cryogenian Argyll Group, it and the overlying units...
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First thumbnail for: Evidence, or not, for the late Tonian break-up of ...
Second thumbnail for: Evidence, or not, for the late Tonian break-up of ...
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Journal Article
Published: 01 December 1999
Journal of the Geological Society (1999) 156 (6): 1163–1173.
...). Grampian Group Glenshirra Subgroup. The Glenshirra Subgroup forms the oldest exposed strata of the Grampian Group. It comprises a distinctive association of pink and grey mainly arkosic psammite with quartzite and minor semipelite which crops out in a number of structural inliers in the Foyers district...
Journal Article
Published: 01 August 1990
Journal of the Geological Society (1990) 147 (4): 732–734.
... et al. 1981, 1983) are currently considered to be part of the Grampian Group on structural and stratigraphic grounds and occur within the Cor- rieyairack Subgroup. Glover & Winchester (1989, page 85, para. 4) ignore the Glenshirra Succession (Haselock et al. 1982). However, in Strathnairn, northeast...
Journal Article
Published: 01 April 2007
Scottish Journal of Geology (2007) 43 (1): 9–14.
.... & WINCHESTER , J.A. 2004 . Sedimentology and stratigraphic affinities of Neoproterozoic coarse clastic successions, Glenshirra Group, Inverness-shire, Scotland . Scottish Journal of Geology , 40 , 159 – 174 . COLLINSON , J.D. & THOMPSON , D.B. 1988 . Sedimentary Structures...
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First thumbnail for: Exceptional preservation of sedimentary structures...
Second thumbnail for: Exceptional preservation of sedimentary structures...
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Journal Article
Published: 01 February 1998
Journal of the Geological Society (1998) 155 (1): 13–24.
... of the Corrieyairack sequence, it is evident that the Glenshirra Sub- group represents an early development of the Grampian rift basin, with a fill at least 2 km thick, and again an east-facing half-graben geometry can be inferred. What then is the likely relationship of the multiple Grampian rift sequence...
Journal Article
Published: 13 September 2024
Journal of the Geological Society (2024) 181 (6): jgs2024-085.
...Fig. 6. Representative sandstones of the (meta)sedimentary units south of the Great Glen Fault that are dominated by 1.8–1.6 Ga detrital zircons: ( a ) Loch Laggan Formation (Grampian Group), Loch Laggan; ( b , c ) Glenshirra Group, Loch Tarff; ( d ) Dun Gallain Formation (upper Colonsay Group...
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First thumbnail for: How great is the Great Glen Fault?
Second thumbnail for: How great is the Great Glen Fault?
Third thumbnail for: How great is the Great Glen Fault?
Journal Article
Published: 01 March 2000
Journal of the Geological Society (2000) 157 (2): 509–510.
... outline with the southern and eastern sides sub‐parallel to the strike of the host rocks and the broad trend of outcrop of the Glenshirra and Corrieyairack sub‐groups of the Grampian Group. These trends are respectively NNW–SSE and east–west, sharply discordant to the NE–SW regional Caledonian strike...
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First thumbnail for: Discussion on the influence of country rock struct...
Journal Article
Published: 01 December 1999
Journal of the Geological Society (1999) 156 (6): 1175–1182.
... and Glen Roy, and an eastern domain extending from the Steep Belt towards Drumochter. The Kinlochlaggan succession separates the two domains north of the River Spey whereas the Inverpattack Markie Fault forms the boundary further south (Fig. 2). The western Grampian Group is divided into the Glenshirra...
Journal Article
Published: 01 March 2003
Journal of the Geological Society (2003) 160 (2): 231–246.
... lithofacies of the Glenshirra Subgroup. It was collected upstream of Garva Bridge at NN 5236 9512. The Glenshirra psammites are lithologically and geochemically distinct from the rest of the Grampian Group, as they formed in shallow marine conditions subject to subaerial erosion, fluviatile deposition and red...
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First thumbnail for: Source of the Dalradian Supergroup constrained by ...
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Journal Article
Published: 01 December 1994
Journal of the Geological Society (1994) 151 (6): 971–986.
... asigned to the Glenshirra Subgroup (Haselock 1982). The structurally and stratigraphically overlying Appin Group has been subdivided into (Harris & Pitcher 1975): (a) the Lochaber Subgroup, a sequence of pelitic to semipelitic schists with thin quartzites towards its base; and (b) the overlying...
Journal Article
Published: 01 April 1995
Journal of the Geological Society (1995) 152 (2): 391–406.
... (Haselock et al . 1982; Phillips et al. 1994). The underlying strata, the Glenshirra Succession have previously been included in the Grampian Group (Haselock & Evans 1990; Glover & Winchester 1990). However, in view of the structural break that exists between the two successions in the study area we...
Journal Article
Published: 01 November 2010
Scottish Journal of Geology (2010) 46 (2): 97–111.
... shallow marine Glen Spean Subgroup ( Banks et al . 2007 ; Fig. 8 ). Some workers also include the Glenshirra Group as the lowermost unit of the Grampian Group ( Robertson & Smith 1999 ; Smith et al . 1999 ; Cawood et al . 2003 ; Fig. 8 ). Basin analysis suggests that the Grampian Group...
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