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Glenelg River Complex

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Figure 1. Cambrian–Ordovician geology of <b>Glenelg</b> <b>River</b> <b>Complex</b> (GRC) showin...
in > Geology
Published: 01 April 2003
Figure 1. Cambrian–Ordovician geology of Glenelg River Complex (GRC) showing main occurrences of boninitic rocks (circled)
Series: Geological Society, London, Special Publications, Geological Society, London, Special Publications
Published: 01 January 2015
DOI: 10.1144/SP413.8
EISBN: 9781862397170
... Abstract Mafic and ultramafic rocks intercalated with metamorphosed deep-marine sediments in the Glenelg River Complex of SE Australia comprise variably tectonized fragments of an interpreted late Neoproterozoic–earliest Cambrian hyper-extended continental margin that was dismembered and thrust...
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Journal Article
Journal: Geology
Published: 01 April 2003
Geology (2003) 31 (4): 371–374.
...Figure 1. Cambrian–Ordovician geology of Glenelg River Complex (GRC) showing main occurrences of boninitic rocks (circled) ...
FIGURES
Journal Article
Published: 21 November 2017
Scottish Journal of Geology (2018) 54 (1): 13–35.
... to Southern Sweden, and is one of the largest collisional belts on Earth (e.g. Rivers 1997 , 2008 ; Tollo et al. 2004 ; Tohver et al. 2004 ). The Archaean–Palaeoproterozoic Glenelg Inlier in Scotland and the Annagh Gneiss Complex in Ireland provide small but crucial links between the North American...
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Journal Article
Published: 01 September 2005
Geological Magazine (2005) 142 (5): 605–615.
..., that is, the Lewisian Complex (Fig. 1 ). The Glenelg–Attadale Inlier contains eclogites and their retrogressed equivalents ( Teall, 1891 ; Peach et al . 1910 ; Alderman, 1936 ; Mercy & O’Hara, 1968 ). Ramsay (1958) and Sutton & Watson (1959) divided the Glenelg–Attadale Inlier into two...
FIGURES
Journal Article
Published: 01 June 1992
Bulletin of Canadian Petroleum Geology (1992) 40 (2): 151–169.
... fields. At Venture, the accumulation is associ- ated with a major rollover anticline into a large listric fault. Glenelg is a complex structure associated with a deep listric fault. Trapping is through fault closure and fault seal under a shale (Naskapi fm) top seal at Glenelg while at Venture topseals...
Journal Article
Journal: Geology
Published: 01 April 2006
Geology (2006) 34 (4): 249–252.
...Don I. Cummings; R. William C. Arnott; Bruce S. Hart Abstract Based on its anomalous thickness (∼150 m) and stratigraphic position above continental-slope mudstone, an upward-coarsening succession consisting in part of tidal rhythmites in the Glenelg Field, offshore Nova Scotia, Canada...
FIGURES
Journal Article
Journal: Geology
Published: 21 July 2020
Geology (2020) 48 (11): 1094–1098.
... ), and the former three show isotopic disturbance at ca. 1740–1600 Ma. The protolith ages support correlation with the foreland Lewisian Gneiss Complex ( Moorbath and Taylor, 1974 ) and a Laurentian affinity. However, greater tectonic complexity is indicated by the presence within the Eastern unit of the Glenelg...
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Journal Article
Published: 01 September 2005
Bulletin of Canadian Petroleum Geology (2005) 53 (3): 211–236.
... of the largest gas accumulations offshore Nova Scotia (Venture, Alma, Glenelg) occur in growth-faulted shelf-margin delta complexes that formed at or near the paleoshelf edge during periods of low relative sea-level. Shelf-margin deltas are excellent exploration targets for several reasons: they commonly have...
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Journal Article
Journal: GSA Bulletin
Published: 01 November 2014
GSA Bulletin (2014) 126 (11-12): 1416–1438.
... of Australia in Antarctica; however, the correlation between lithotectonic units in Antarctica (Wilson, Bowers, and Robertson Bay terranes) and those in southeastern Australia (Glenelg, Grampians-Stavely, and Stawell zones), as well as the presence of Lachlan-aged tectono-metamorphic events in northern...
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Journal Article
Journal: AAPG Bulletin
Published: 01 July 2004
AAPG Bulletin (2004) 88 (7): 991–1006.
...David J. W. Piper; Georgia Pe-Piper; Stephen C. Ingram Abstract Conventional cores from Lower Cretaceous outer-shelf and upper-slope prodelta facies in the Alma and Glenelg fields of the Scotian Basin show a wide range of synsedimentary deformation. Storm-dominated prodelta sandstone and mudstone...
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Journal Article
Published: 25 November 2012
Canadian Journal of Earth Sciences (2012) 49 (12): 1417–1462.
... multidisciplinary biostratigraphic studies of the Mesozoic sections in eight wells: Bonnet P-23, Chebucto K-90, Cohasset L-97, Glenelg J-48, Glooscap C-63, Mohican I-100, South Desbarres O-76, and South Griffin J-13. These wells were chosen to provide good spatial coverage, stratigraphic penetration...
Journal Article
Journal: AAPG Bulletin
Published: 15 February 2019
AAPG Bulletin (2019) 103 (2): 433–467.
.... The use of multidisciplinary constraints (geomorphology, geology, geophysics) in forward stratigraphic models sheds light on the complex interaction of local, regional, and global driving mechanisms that influence sediment transport and deposition along continuously evolving landscapes. In this paper, we...
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Journal Article
Published: 01 May 2011
Scottish Journal of Geology (2011) 47 (1): 1–20.
... et al . 2006 ). Which of these thrusts links with the Sgurr Beag Thrust remains uncertain, in part because the distinction between the Morar, Glenfinnan and Loch Eil groups in this area is obfuscated by structural complexity and high-grade metamorphism ( Strachan & Holdsworth 1988 ; Kocks et al...
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Series: Geological Society, London, Special Reports, Geological Society, London, Special Reports
Published: 01 January 1994
DOI: 10.1144/SR22.2
EISBN: 9781786202857
... Abstract The Precambrian foreland rocks, lying west of the Moine Thrust Zone of northwest Scotland, consist of a crystalline, mainly gneissose, basement (the Lewisian complex) overlain by an undeformed or gently tilted sedimentary cover (the Torridonian). This chapter provides an overview...
Journal Article
Published: 01 March 2016
Journal of Sedimentary Research (2016) 86 (3): 199–216.
... point to significant morphodynamic complexity and geomorphic variability, challenging the assumption that all pre-Silurian rivers shared poor channelization and low sinuosity. Observed channel bodies also have width:thickness ratios strongly overlapping with those of rivers postdating the rise...
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Journal Article
Published: 01 March 1980
Bulletin of Canadian Petroleum Geology (1980) 28 (1): 59–79.
... of these implications have now been accounted for in the published facies-model package, but the problem is that rivers represent a particularly complex multivariate nvironment in which there are many sedimentary feed-back effects, and several facies groupings or sequences can be arrived at in more than one way...
Journal Article
Published: 01 September 1976
Bulletin of Canadian Petroleum Geology (1976) 24 (3): 321–371.
... Christopher et Hassel d’âge Albien, et Kanguk, d’âge Santonien à Maastrichtien, cette dernière ayant pu être divisée en trois membres. Enfin, dans l’Anderson Plain, sur le continent Canadien, l’examen détaillé des coupes de Horton River pour le Crétacé inférieur et d’Anderson River pour le Crétacé supérieur...
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Figure 3. Primitive mantle–normalized (values from  McDonough and Sun, 1995...
in > Geology
Published: 01 April 2003
Figure 3. Primitive mantle–normalized (values from McDonough and Sun, 1995 ) multielement diagram for Glenelg River Complex boninitic diorites (Mg# in brackets). Hornblende diorite lacks hybridization textures and phenocrysts. Data sources: Setouchi volcanic belt, Tatsumi and Ishizaka (1982
Journal Article
Published: 01 June 1993
Journal of the Geological Society (1993) 150 (3): 447–464.
...G. ROGERS; R.J. PANKHURST Abstract The paper by Giletti et al. 1961 is seen as a major landmark in the evolution of dating techniques in polymetamorphic terrains. We consider certain critical issues from each of the main complexes of the Scottish Highlands studied by Giletti et al. to illustrate...