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Eriboll Formation

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Journal Article
Published: 01 May 2011
Scottish Journal of Geology (2011) 47 (1): 45-56.
...J. N. Hooker; S. E. Laubach; L. Gomez; R. Marrett; P. Eichhubl; K. Diaz-Tushman; E. Pinzon AbstractSynopsisWe investigated fracture intensity of the Cambrian Eriboll Formation sandstone exposures west of the Palaeozoic Moine Thrust Belt (MTB) in NW Scotland, by measuring the number and size...
FIGURES
Journal Article
Published: 01 March 2009
Journal of the Geological Society (2009) 166 (2): 349-362.
...S.E. Laubach; Kira Diaz-Tushman Abstract:Cambrian Eriboll Formation sandstones of the Ardvreck Group that crop out west of the Moine Thrust Zone contain joints and quartz-filled or quartz-lined fractures that resemble cemented joints. Of the fractures containing quartz, five sets strike north, NW...
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Fractures in <b>Eriboll</b> <b>Formation</b> exposures and scan line procedure. ( a ) Fra...
Published: 01 May 2011
Fig. 2 Fractures in Eriboll Formation exposures and scan line procedure. ( a ) Fracture traces, east-dipping bed surface, view to north from near Loch an Nid [NH077 746]. ( b ) Scan line (red line with gap) and quartz-filled set A fracture; opening displacement (kinematic aperture) is measured
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Fracture sets containing quartz mineralization, <b>Eriboll</b> <b>Formation</b> sandstone...
Published: 01 March 2009
Fig. 9. Fracture sets containing quartz mineralization, Eriboll Formation sandstone, west of the Moine Thrust Zone.
Journal Article
Published: 01 May 2012
Journal of the Geological Society (2012) 169 (3): 297-310.
...–wing crack arrays that formed progressively; these are more abundant near small-displacement, oblique-slip faults that offset the overlying Cambrian Eriboll Formation and the Moine Thrust Belt. Applecross sandstones have low fracture abundance, possibly a consequence of low elastic moduli (Young’s...
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Journal Article
Published: 29 September 2017
Journal of the Geological Society (2017) 175 (1): 33-43.
...John Parnell; Stephen Bowden; Darren Mark AbstractFluid inclusion and organic biomarker data show that there was formerly a hydrocarbon system in the Cambro-Ordovician Laurentian margin rocks of NW Scotland. Oil fluid inclusions occur in stylolitized Eriboll Formation sandstone, in K-feldspar...
Series: AAPG Memoir
Published: 01 January 1969
DOI: 10.1306/M12367C45
EISBN: 9781629812274
... front of the transgression. A revised composite thickness of more than 4,000 ft is offered for the Eriboll Sandstone, the An t-Sron Formation, and the Durness Carbonate, which successively overlie the unconformity. The progression of the miner- alogic and textural parameters of the succession toward...
Series: Geological Society, London, Special Publications
Published: 01 January 2000
DOI: 10.1144/SR24.12
EISBN: 9781862396920
... extends for nearly 200 km, from Eriboll in the north to Skye in the south. The Durness Group is most completely preserved in a half-graben at Durness. Peach et al. (1907) described the Geological Survey’s detailed mapping of the north-west highlands (see Oldroyd 1990), the basis for all subsequent work...
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Fracture abundance in Applecross <b>Formation</b> sandstone compared with that of ...
Published: 01 May 2012
Fig. 17. Fracture abundance in Applecross Formation sandstone compared with that of Eriboll Formation. ( a ) Fracture length v. distance, late ENE–WSW-striking fractures, Eriboll Formation, showing numerous mostly short fractures. ( b ) Fracture length v. distance, in Applecross Formation, along
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Figure 8. Reconstruction of the northeast Laurentian and West Baltica margi...
Published: 01 July 2007
to the Eriboll Formation, and D1 is a position to the south based on possible subsequent strike slip on intervening structures that would have displaced outboard units along the Laurentian margin and Baltica northward with respect to cratonic Laurentia (cf. Dewey and Strachan, 2003 ). Abbreviations: D—Dalradian
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Diagrams showing the paragenetic relationships in three lithologies (vein-f...
Published: 01 December 2005
Fig. 11.  Diagrams showing the paragenetic relationships in three lithologies (vein-filling in Torridon Group sandstone, cement and veining in Eriboll Formation sandstone, mineralized Durness Group limestone) that are dominated by the Component 1 magnetization. The petrographical relationships
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Exposures of Applecross sandstone pavements having low overall fracture abu...
Published: 01 May 2012
Fig. 4. Exposures of Applecross sandstone pavements having low overall fracture abundance. ( a ) Applecross sandstone (Ax), Eriboll Formation (E), and faults (f) near NH0984. Airphotograph. Bing. ( b ) Applecross Formation outcrops. View NW of [NH09788374]. (Note figure and tents for scale.) ( c
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Faults, geology and key localities east of An Teallach. Bold black lines in...
Published: 01 May 2012
. E, Eriboll Formation: yellow, Basal Quartzite Member; blue, Pipe Rock Member. Key exposure prefixes: A, Set A scanlines; B, Set B scanlines; S, Set L scanlines.
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Figure 3. Stratigraphic columns for the Ardvreck Group, Scotland, the Treka...
Published: 01 July 2007
Figure 3. Stratigraphic columns for the Ardvreck Group, Scotland, the Trekant and Zebra Series, East Greenland, and the Labrador Group, West Newfoundland. Vertical lines within sandstone units in Eriboll Formation, Zebra Series, and Bradore Formation schematically illustrate the presence
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Figure 6. Probability density distribution diagram of siliciclastic sequenc...
Published: 01 July 2007
, and South Brook Formations, West Newfoundland— Cawood and Nemchin (2001) ; Green Beds and Keltie Water Grit, Southern Highland Group, northwest Scotland— Cawood et al. (2003) ; Basal Quartzite and Pipe Rock Members, Eriboll Formation, Ardvreck Group, northwest Scotland—Cawood et al. (this paper); Zebra
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Probability plots of Neoproterozoic and early Palaeozoic metasedimentary un...
Published: 01 March 2007
. (2003) ; Eriboll Formation (Ardvreck Group), P. A. Cawood et al . (unpubl. data). s, number of samples; n, number of analyses.
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Probability plots of latest Neoproterozoic to early Palaeozoic metasediment...
Published: 01 March 2007
(including Eastern and Central Blue Ridge, Dahlonega gold belt, Sauratown Mountains window and Smith River Allochthon), Bream et al . (2004) and Carter et al . (2006) ; Hebridean Foreland (Eriboll Formation, Ardvreck Group), P. A. Cawood et al . (unpubl. data); Newfoundland (Bradore, Hawke Bay
Journal Article
Journal: GSA Bulletin
Published: 01 July 2007
GSA Bulletin (2007) 119 (7-8): 993-1003.
... to the Eriboll Formation, and D1 is a position to the south based on possible subsequent strike slip on intervening structures that would have displaced outboard units along the Laurentian margin and Baltica northward with respect to cratonic Laurentia (cf. Dewey and Strachan, 2003 ). Abbreviations: D—Dalradian...
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Series: Geological Society, London, Special Publications
Published: 01 January 2010
DOI: 10.1144/SP335.26
EISBN: 9781862395831
... Table 1. Method 1 vorticity estimates (W m ) from mylonitic Moine psammite and Lewisianoid basement from the Moine Nappe and mylonitic Oystershell Rock and Eriboll Formation from the Creagan thrust sheet. Great Britian (GB) National Grid Coordinates obtained using WAAS (Wide Area...
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Comparisons of the Proterozoic–Lower Palaeozoic stratigraphy in the parauto...
Published: 01 March 2001
stratigraphy of the fjord zone for comparison. CL: Charcot Land supracrustal sequence (includes volcanics). D: Durness Group. E: Eriboll and An t-Sròn formations. EBS: Eleonore Bay Supergroup. ES: Eleonore Sø volcano-sedimentary complex. HF: Hagen Fjord Group. HG: Hamberg Gletscher foreland complex. HS: Hekla