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Craven inliers

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The <b>Craven</b> <b>Inliers</b> and their regional setting. Based on Arthurton  et al . ...
Published: 01 May 2013
Fig. 1. The Craven Inliers and their regional setting. Based on Arthurton et al . ( 1988 , fig. 3).
Image
Interpretive subcrop map of the western <b>Craven</b> <b>inliers</b> (Silurian stratigrap...
Published: 01 November 2005
Fig. 12. Interpretive subcrop map of the western Craven inliers (Silurian stratigraphy simplified). Sub-Carboniferous crop of selected boundaries dotted.
Journal Article
Published: 01 November 2005
Proceedings of the Yorkshire Geological Society (2005) 55 (4): 241-261.
...Fig. 12. Interpretive subcrop map of the western Craven inliers (Silurian stratigraphy simplified). Sub-Carboniferous crop of selected boundaries dotted. ...
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Journal Article
Published: 01 May 2013
Proceedings of the Yorkshire Geological Society (2013) 59 (3): 173-176.
...Fig. 1. The Craven Inliers and their regional setting. Based on Arthurton et al . ( 1988 , fig. 3). ...
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Series: Geological Society, London, Special Reports
Published: 01 January 2011
DOI: 10.1144/SR26.11
EISBN: 9781862396944
.... Geological map showing the distribution of Carboniferous strata of the Craven Basin and southern Pennines, adapted from IGS (1979). Namurian strata occur at outcrop along the axis of the Pennine Anticline, in the Rossendale Anticline and flanking the Craven inlier of Tournaisian and Visean strata (Fig...
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Journal Article
Published: 02 May 2019
Petroleum Geoscience (2019) petgeo2018-039.
... lithological descriptions of seven lithofacies, XRD mineralogy and hydrocarbon-specific geochemical data for 32 outcrop localities within the Craven and Edale basins, respectively in the northern and southern parts of the resource area. Low oxygen indices suggest that the majority of samples are relatively...
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Journal Article
Published: 01 November 2015
Proceedings of the Yorkshire Geological Society (2015) 60 (4): 258-274.
... wedge of Silurian strata lies between them near the branch point. The two faults swing southeastward, joining the Craven fault system via splays and linkages. Regionally, the Dent and Barbon faults form the innermost pair of a fan of ~N–S striking faults splaying off the northwest end of the South...
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Journal Article
Published: 01 November 2000
Proceedings of the Yorkshire Geological Society (2000) 53 (2): 119-128.
...), shelf facies at the southern end of the Askrigg Block (stippled), basin facies (unpatterned), the Lower Palaeozoic inlier (vertically ruled), and the Craven Faults. Namurian outcrops have been omitted for clarity. Sponge-bearing framework facies are exposed at the numbered locations: (1) High Hill...
Journal Article
Published: 22 February 2016
Geological Magazine (2016) 154 (2): 305-333.
... and in a series of inliers located adjacent to the North Craven Fault ( Fig. 1 ). One of the main aims of this study is to provide a single unified nomenclature for the southern part of the Askrigg Block, associated with the development of a carbonate succession on the tilt-block high. This has...
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Series: Geological Society, London, Special Publications
Published: 01 January 2000
DOI: 10.1144/SR24.8
EISBN: 9781862396920
... Abstract In northern England Ordovician rocks crop out in the main Lake District inlier and in smaller inliers at Cross Fell, Cautley, Austwick and Teesdale (Fig.1), where they are brought up along the Pennine, Dent and Craven fault systems. The Lake District has a thick lower Ordovician...
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SW part of the Askrigg Block, northern England, bounded by the <b>Craven</b> and D...
Published: 01 November 2005
Fig. 1. SW part of the Askrigg Block, northern England, bounded by the Craven and Dent fault systems, showing the Craven inliers. Lower Palaeozic rocks stippled, Ingleton Group black. Sub-Carboniferous crop and concealed extent of the Wensleydale Granite, and positive aeromagnetic anomaly in nT
Journal Article
Published: 17 February 2017
Proceedings of the Yorkshire Geological Society (2017) 61 (3): 179-196.
...), forms a series of inliers located south of the North Craven Fault, along a roughly E–W-trending tract extending 20 km eastwards from Settle to Burnsall ( Fig. 1 ). The formation is recognized as comprising mainly Cracoean reefs that formed an abrupt southern margin to the Askrigg Block carbonate shelf...
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Journal Article
Journal: Economic Geology
Published: 01 December 2016
Economic Geology (2016) 111 (8): 2087-2109.
...N. Hayward; L. Corriveau; J. A. Craven; R. J. Enkin Abstract Models of the three-dimensional physical property variation of the NICO Au-Co-Bi-Cu deposit, Northwest Territories, and the Southern Breccia albitite-hosted uranium occurrences and their iron oxide-alkali alteration envelopes, were...
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Journal Article
Published: 01 December 1988
Journal of the Geological Society (1988) 145 (6): 925-933.
...N. H. WOODCOCK Abstract The Old Radnor Inlier comprises Precambrian sediments unconformably overlain by Wenlock age limestones and shales. Its structure is dominated by steep strike-slip faults. Major NE-SW faults probably bound the inlier and are linked by more northerly faults to form a strike...
Series: Geological Society, London, Special Publications
Published: 01 January 2002
DOI: 10.1144/GSL.SP.2002.201.01.04
EISBN: 9781862394490
...) pronounced subsidence occurred associated with back-arc rifting. During the Silurian (443-417 Ma) development of a foreland basin is deduced from the convex upwards curves in the Lake District and also in the Craven Inlier. At the same time extensional basins with concave upwards subsidence curves developed...
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Series: Geological Society, London, Special Reports
Published: 01 January 2011
DOI: 10.1144/SR26.10
EISBN: 9781862396944
... rocks pass into more basinal successions in the Edale Basin to the north, the Widmerpool Gulf to the south and the Staffordshire Basin to the west, dominated by hemi-pelagic mudstone and carbonate turbidites (Craven Group). The lithostratigraphical nomenclature for the Tournaisian and Visean strata...
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Journal Article
Published: 14 November 2008
Geological Magazine (2008) 146 (2): 237-251.
... is a tightly folded sequence of mudstone, wacke and sporadic conglomerate of possible Precambrian or Early Ordovician age that crops out within the Craven inliers at Ingleton and in Ribblesdale, northwest Yorkshire (Soper & Dunning, 2005 ; Williamson, 2005 ). The group is unconformably overlain by strata...
Journal Article
Published: 01 November 1984
Journal of the Geological Society (1984) 141 (6): 1001-1014.
...N. H. Woodcock Abstract The NE-trending Pontesford Lineament centres on the Pontesford-Linley and adjacent faults in the Shelve/Longmynd inlier. To the NE it is usually drawn along the SE edge of the Cheshire Basin and to the SW along a variety of lines parallel to or converging with the Church...
Journal Article
Published: 22 March 2016
Proceedings of the Yorkshire Geological Society (2016) 61 (1): 55-86.
... along the eastern margins of a large inlier, the Derbyshire High, in Carboniferous platform carbonate host rocks. The inlier covers some 390 km 2 , forms an up-dip promontory of a larger structure, the East Midlands Shelf, and is surrounded by shales and sandstones of the Millstone Grit and Pennine Coal...
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Series: Geological Society, London, Special Reports
Published: 01 January 2011
DOI: 10.1144/SR26.9
EISBN: 9781862396944
... (Millstone Grit Group) (Fraser & Gawthorpe 2003). The oldest Carboniferous strata of late Tournaisian to Visean age do not crop out widely in the region, but are known from boreholes and geophysical records in South Derbyshire and the Vale of Belvoir, and from small inliers in Shropshire and the Clee...
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