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Wales-Brabant High

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Journal Article
Published: 06 September 2017
Proceedings of the Yorkshire Geological Society (2017) 61 (4): 285-309.
... to the south on the Wales-Brabant High. Monazite is common in northern sandstones, whereas it is rare in southern sandstones. Southern sandstones may also contain chrome spinel: variations in its abundance identify spatial and temporal variations in the southern supply. There is evidence in some sandstones...
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Journal Article
Published: 01 May 2005
Proceedings of the Yorkshire Geological Society (2005) 55 (3): 209-233.
... source region was situated not far to the south of the basin, probably in the part of eastern Avalonia that included the WalesBrabant High. Local sediment from different parts of this area was incorporated into both the westerly and northerly derived supplies at intervals through Namurian...
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Image
Location of study area relative to Pennine Basin and <b>Wales</b>–<b>Brabant</b> <b>High</b>. Pa...
Published: 01 May 2005
Fig. 1. Location of study area relative to Pennine Basin and WalesBrabant High. Palaeogeography of the early Westphalian after Guion (1992 ). Yorkshire study area ( Hallsworth & Chisholm 2000 ) also shown. L, Leeds; MV, Merevale Borehole; N, Nottingham.
Series: Geological Society, London, Special Reports
Published: 01 January 2011
DOI: 10.1144/SR26.8
EISBN: 9781862396944
...-to-shelf carbonates, present along the northern margin of the Wales-Brabant High, extending across North Wales (Clwyd Limestone Group). Visean to Namurian basinal deposits (Craven Group) occur on the north coast of North Wales (Fig. 25), deposited on the southern margin of the Irish Sea Basin (see Chapter...
FIGURES
Series: Geological Society, London, Special Reports
Published: 01 January 2011
DOI: 10.1144/SR26.7
EISBN: 9781862396944
... coalfields, with progressively younger successions onlapping northwestwards onto the southern flank of the Wales-Brabant High. Pre-Asturian fluvio-lacustrine deposits (South Wales Coal Measures Group) are present in the Berkshire and Kent coalfields, but are restricted to isolated inliers beneath Asturian...
FIGURES
Journal Article
Published: 01 May 2006
Proceedings of the Yorkshire Geological Society (2006) 56 (1): 15-30.
... proximal to the Variscan Front (South Wales, Kent), varied cleat azimuths provide evidence of stress deflection and block rotation, whereas north of the Wales-Brabant High (central and northern England), a consistent regional north-westerly maximum horizontal stress is indicated by regionally parallel...
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Series: Geological Society, London, Special Reports
Published: 01 January 2011
DOI: 10.1144/SR26.15
EISBN: 9781862396944
... between the Mid North Sea High to the north and the Wales-Brabant High to the south (Fig. 46). It is laterally contiguous with the Pennine Basin complex. An isolated area of Carboniferous strata has also been proved in the Clair Basin of the NW Approaches, west of the Shetland Isles. The Tournaisian...
FIGURES
Journal Article
Published: 01 May 2008
Proceedings of the Yorkshire Geological Society (2008) 57 (1): 1-28.
...-slope deposits to mouthbar and channel sandstones. The latter comprises an ‘eastern inflow’ of northerly provenance, the distribution of which was not influenced by the underlying basement configuration, and a ‘southern inflow’ sourced from the Wales-Brabant High. Falling sea-levels resulted...
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Series: Geological Society, London, Special Publications
Published: 01 January 2002
DOI: 10.1144/GSL.SP.2002.201.01.04
EISBN: 9781862394490
... and the neighbouring palaeocontinents Baltica, Gondwana and Laurentia. From Cambrian to Tremadocian time Avalonia was attached or close to northern Gondwana, with, in the Cambrian, a very high latitude position and in the Tremadocian, an approximately 60° south position for Wales. By Llanvirn time Avalonia was moving...
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Journal Article
Published: 01 January 2014
Journal of the Geological Society (2014) 171 (1): 41-47.
...-level cycle in carbonate ramp to basinal settings of the WalesBrabant massif, British Isles . Sedimentary Geology , 284–285 , 197 – 213 . Beus S.S. 1984 . Fossil associations in the High Tor Limestone (Lower Carboniferous) of South Wales . Journal of Paleontology , 58 , 651 – 667...
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Journal Article
Published: 01 December 1993
Journal of the Geological Society (1993) 150 (6): 1121-1136.
...A. J. HARTLEY Abstract Mid-Westphalian A to late Westphalian B sediments of the South Wales Coalfield comprise mainly lacustrine, raised mire and flood deposits developed in an upper coastal plain environment. Occasional high sinuosity, fine-grained channel systems drained the subdued topography...
Journal Article
Published: 01 November 2007
Quarterly Journal of Engineering Geology and Hydrogeology (2007) 40 (4): 417-434.
... of carbonate mudstones, wackestones and packstones. The compact, oolitic limestones that form much of the formation have low primary intergranular porosity and permeability, whereas high secondary fissure and micro-fissure permeabilities are present throughout much of the formation, being associated...
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Journal Article
Published: 01 March 2003
Journal of the Geological Society (2003) 160 (2): 219-229.
.... It was, probably, a continent–continent collision to the south of Wales and the Brabant Massif, perhaps a westward continuation of the Armorican and Bohemian Massifs, like that of the Northern Appalachians ( Soper et al . 1992 ). The evidence is now disjunct, because, from Cornubia to the Ardennes, deep-water...
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Journal Article
Published: 01 May 2015
Proceedings of the Yorkshire Geological Society (2015) 60 (3): 204-226.
... of the Northwest European Carboniferous Basin ( Ziegler 1990 ). To the east, coals in the Netherlands, Belgium and the Ruhr belong to the same basin. South of the Pennine Basin, the Wales-Brabant High extends to the SE ( Fig. 1 ). The definition of the southern margin of the basin owes much to the pioneering work...
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Journal Article
Published: 01 November 2012
Journal of the Geological Society (2012) 169 (6): 713-721.
... of Northwest Europe . Blackie , Glasgow , 153 – 177 . Guion P.D. Fulton I.M. Jones N.S. 1995 . Sedimentary facies of the coal-bearing Westphalian A and B north of the WalesBrabant High . In : Whateley M.K.G. Spears D.A. (eds) European Coal Geology . Geological...
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Journal Article
Published: 01 November 2001
Journal of the Geological Society (2001) 158 (6): 983-994.
...A. ZEH; H. BRÄTZ; I. L. MILLAR; I. S. WILLIAMS Abstract Abstract: SHRIMP analyses of detrital zircon cores from high-grade metasediments from the Mid-German Crystalline Rise, which is situated between Eastern Avalonia in the NW and Saxo-Thuringia in the SE, yield mostly ages of c. 550 Ma and c...
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Journal Article
Published: 01 March 2011
Journal of the Geological Society (2011) 168 (2): 407-422.
...Koen Van Noten; Philippe Muchez; Manuel Sintubin Abstract: In the frontal part of the Rhenohercynian fold-and-thrust belt (High-Ardenne slate belt, Germany), two successive types of quartz veins, oriented normal and parallel to bedding respectively, are interpreted to reflect the early Variscan...
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Generalized transport paths to southern part of Pennine Basin during Namuri...
Published: 01 May 2005
Fig. 13. Generalized transport paths to southern part of Pennine Basin during Namurian to mid-Duckmantian times. 1A, northern provenance, main transport route from north; IB, northern provenance, eastern supply route with local additions from WalesBrabant High; 2, western provenance with local
Image
Maps showing the possible distribution of sediment lobes extending into the...
Published: 06 September 2017
Fig. 9. Maps showing the possible distribution of sediment lobes extending into the depositional regions north of the Wales-Brabant High, based on heavy mineral ratios (see Appendix A ) and palaeocurrent data ( Tables 1 and 2 ). The Kinderscoutian map is based partly on Aitkenhead et al
Image
Maps showing the possible distribution of sediment lobes extending into the...
Published: 06 September 2017
Fig. 9. Maps showing the possible distribution of sediment lobes extending into the depositional regions north of the Wales-Brabant High, based on heavy mineral ratios (see Appendix A ) and palaeocurrent data ( Tables 1 and 2 ). The Kinderscoutian map is based partly on Aitkenhead et al