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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, Geological Society, London, Special Reports
Published: 01 January 2011
DOI: 10.1144/SR26.8
EISBN: 9781862396944
... the northward progradation of fluvio-deltaic facies deposited along the northern margin of the Wales-Brabant High. South of the Bala Fault, the Cefn-y-fedw Sandstone Formation occurs as a single, thick sandstone succession (Fig. 26 , Cols 8 & 9) and conformably overlies the Visean Minera Formation...
FIGURES
Series: Geological Society, London, Special Reports, Geological Society, London, Special Reports
Published: 01 January 2011
DOI: 10.1144/SR26.7
EISBN: 9781862396944
... within the region. Westphalian strata are proved in all three coalfields, with progressively younger successions onlapping north-westwards 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...
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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, Geological Society, London, Special Reports
Published: 01 January 2011
DOI: 10.1144/SR26.15
EISBN: 9781862396944
... to Brigantian foraminifers occur in Quadrant 38 O2 . In the Southern North Sea Arundian to Arnsbergian miospores are present in Quadrant 41 (Fig. 47 , Col. 6 ^1 ). Visean shallow marine platform carbonates are developed along the margin of the Wales-Brabant Massif on the Hewett Shelf and Winterton High...
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Journal Article
Published: 26 January 2021
Proceedings of the Yorkshire Geological Society (2021) 63 (3): pygs2020-010.
... and location of the source areas that supplied the clastic sediment. The study confirms that most sandstones were derived from distant areas to the north, west and south, and that a local source, in the WalesBrabant High, also supplied sediment at times. The northern sources are thought to lie mainly...
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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, Geological Society, London, Special Publications
Published: 01 January 2002
DOI: 10.1144/GSL.SP.2002.201.01.04
EISBN: 9781862394490
... Abstract A review is given of recently published and new data on Avalonia east of the Midlands Microcraton. The three megasequences from Cambrian to mid Devonian described in Wales and Welsh Borderland are also present east of the Midlands Microcraton (Brabant Massif, Condroz, Ardennes...
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Journal Article
Published: 30 September 2013
Journal of the Geological Society (2014) 171 (1): 41–47.
... signature of the Tournaisian/Viséan (Lower Carboniferous) sea-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...
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Journal Article
Published: 01 December 1993
Journal of the Geological Society (1993) 150 (6): 1121–1136.
... 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 of the Wales-Brabant Massif to the north and east of the basin. Low...
Journal Article
Published: 01 November 2007
Quarterly Journal of Engineering Geology and Hydrogeology (2007) 40 (4): 417–434.
..., flushing out high-nitrate water found in this zone. This process is conceptually similar to that reported for Pleistocene sand, loam and gravel aquifers in the Noord-Brabant region of the Netherlands, where the poor chemical condition of shallow groundwater leads to exceedance of quality standards...
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Journal Article
Published: 01 March 2003
Journal of the Geological Society (2003) 160 (2): 219–229.
... ). It is not clear what caused the Acadian deformation. 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...
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Journal Article
Published: 21 May 2015
Proceedings of the Yorkshire Geological Society (2015) 60 (3): 204–226.
... 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 of Wills (1956) , who...
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Journal Article
Published: 01 November 2012
Journal of the Geological Society (2012) 169 (6): 713–721.
... 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 Society, London, Special Publications , 82 , 45 – 78 . Gulbranson E.L. Montañez I.P. Schmitz M.D. Limarino C.O...
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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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