Kempsey Beds

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Journal Article
Journal: Lithosphere
Publisher: GSW
Published: 01 December 2016
Lithosphere (2016) 8 (6): 684–698.
... block). Focusing on the lower sedimentary succession within the Nambucca block (Kempsey beds), we recognize two facies associations. Facies association A comprises conglomerate and gravelly sandstone with minor sandstone, collectively interpreted as the deposits of coastal to subaqueous marine fans...
Journal Article
Published: 01 September 1966
Journal of Sedimentary Research (1966) 36 (3): 719–732.
...John F. Lindsay Abstract Unsorted sediments in the Carboniferous Kullatine formation, previously considered tillites, are here defined as subaqueous mudflows. The lensoidal nature of the beds, the general lack of lateral continuity, and the presence of large contorted masses of underlying sediments...
Series: AAPG Methods in Exploration, AAPG Methods in Exploration
Published: 01 January 2002
DOI: 10.1306/Mth13780C18
EISBN: 9781629810584
... lithostratigraphic units several hundred meters thick to marker beds only a few meters thick. Gamma-ray and spectral gamma-ray logs indicate the bulk chemical composition of the rocks, and show that some ignimbrite sheets are internally homogeneous, whereas others are zoned geochemically. Detailed comparison...
FIGURES | View All (14)
Series: Geological Society, London, Special Publications, Geological Society, London, Special Publications
Published: 01 January 2009
DOI: 10.1144/SP313.5
EISBN: 9781862395619
... in the north of the district. Seismic reflection data also reveal strong reflectors that may be halite beds. The area of halite deposition was probably controlled by the Smite and Inkberrow faults, which may be borne out by the absence of salt in the Kempsey borehole to the west of the Smite-Pirton-Tewkesbury...
FIGURES | View All (20)
Journal Article
Published: 01 August 1988
Journal of the Geological Society (1988) 145 (4): 519–522.
.... The interpretation is reasonably well constrained by outcrop and borehole information. At the west end of the section the Collington Borehole penetrates to near the base of the Palaeozoic sequence, beneath the Worcester Basin the Kempsey Borehole (Whittaker et al. 1980) penetrates to the Precambrian basement...
Journal Article
Published: 01 February 1985
Journal of the Geological Society (1985) 142 (1): 187–202.
... geology of the Malvern. Abberley and Ledbury Hills Q J geol Soc London 1969 125 1 37 Poole, E. G. & Williams, B. J. 1981. The Keuper Saliferous Beds of the Droitwich area. IGS Report 81/2. Reading H. G. Poole A. B. A Llandovery shoreline from the southern Malverns Geol Mag...
Series: Geological Society, London, Special Publications
Published: 01 January 2019
DOI: 10.1144/SP471.6
EISBN: 9781786204103
...; CF, Clopton Fault; OTB, Oxfordshire Thrust Belt. As noted earlier, the Silurian beds seen to the west of the Malverns on Figures 6 and 7 show no evidence of thinning towards the present-day Worcester Graben, and it seems reasonable to suppose that they continued across to link up...
FIGURES | View All (15)
Journal Article
Published: 01 January 2008
Journal of the Geological Society (2008) 165 (1): 129–140.
... of diamictites (poorly sorted terrigenous clastic sedimentary rocks with a wide range of grain size), sedimentary intrusions, rhythmites (alternating well-sorted laminae or beds of fine- and coarser-grained lithologies, with or without isolated, dispersed gravel), laminated mudrocks with outsized dispersed...
Series: Geological Society, London, Special Reports, Geological Society, London, Special Reports
Published: 01 January 1994
DOI: 10.1144/SR22.10
EISBN: 9781786202857
...; Bl, Bletchley 1; BT, Bryn-teg; Co, Collington; CS, Church Stretton 1-5; CW, Coxs Walk 1; Ea, Eakring 146; Ed, Edgmond 1; Gl, Glinton 1; GO, Great Osgrove Wood 1; GSt2, Gas Stamford 2; GStlO, Gas Stamford 10; HF, Heath Farm 1; Ho, Hollowell 1; Ke, Kempsey 1; Li, Lilleshall 5; MQ, Morley Quarry 1; NC...
Journal Article
Published: 01 April 1997
Journal of the Geological Society (1997) 154 (2): 225–237.
... foreland during the Carboniferous from microstructural analysis in the British Isles Tectonophysics 1990 177 1 13 Besly B. M. Besly B.M. Kelling G. Palaeogeographic implications of late Westphalian to early Permian red-beds. Central England Sedimentation in a syn-orogenic basin...
Journal Article
Published: 01 February 2009
Journal of Sedimentary Research (2009) 79 (2): 56–82.
.... 1 ). Paleocurrent data were collected from sedimentary structures, such as ripple cross-lamination, cross-bedding, clast imbrication, and symmetrical wave ripples. The collection of statistically significant clast-orientation data within diamictite units for clast-fabric analysis ( sensu Dowdeswell...
FIGURES | View All (15)
Series: Geological Society, London, Geology of Series, Geological Society, London, Geology of Series
Published: 01 January 2006
DOI: 10.1144/GOEWP.2
EISBN: 9781862393882
... Lineament ( Fig. 2.1 ). It includes two major outcrops of volcano- sedimentary sequences and plutonic intrusions, at Charnwood Forest and Nuneaton. In addition, core from the Kempsey and Withycombe Farm boreholes demonstrate its southerly extent. The thick Proterozoic succession at Charnwood Forest...
FIGURES | View All (14)
Journal Article
Published: 01 February 1996
Journal of the Geological Society (1996) 153 (1): 17–32.
...: Proceedings of the 4th conference 1993 London Geological Society 707 716 Besly. B.M. 1983. The sedimentologv and stratigraphy of red beds in the Westphalian A to C of Central England. PhD thesis, University of Keele Besly B.M. Besly B.M. Kelling G. Palaeogeographical...
Journal Article
Journal: Clay Minerals
Published: 01 March 2005
Clay Minerals (2005) 40 (1): 43–61.
... a series of intermediate illite-smectite (I-S) mixed-layer minerals. Progress of this series of dehydration reactions increases the density of the mudstone by mobilizing fluids, and also reducing pore-space as a new, bedding-parallel illite invades and fills voids ( Merriman & Peacor, 1999...
FIGURES | View All (10)
Journal Article
Published: 01 November 2001
Geological Magazine (2001) 138 (6): 669–685.
... by the Kempsey borehole to be Precambrian volcaniclastic rocks of acid to intermediate composition ( Barclay et al. 1997 ). There is also a well-defined residual gravity lineament extending in a NW direction from the area of the Pewsey Faults, which turns to a N–S orientation in the axis of the graben...
FIGURES | View All (9)
Journal Article
Journal: SEG Discovery
Published: 01 July 2013
SEG Discovery (2013) (94): 1–60.