- Page 1: A lithostratigraphical framework fo
- Page 5 and 6: Foreword This report is the publish
- Page 7 and 8: Contents Navigating the document (f
- Page 9: Summary The Stratigraphy Committee
- Page 12 and 13: SOUTHERN UPLAND FAULT IRISH SEA N L
- Page 14 and 15: into a deep marine Culm Basin assoc
- Page 16 and 17: 54°N Volcanic rocks Culm Supergrou
- Page 18 and 19: Table 3 Summary of the chronostrati
- Page 20 and 21: Table 4 Westphalian chronostratigra
- Page 22 and 23: present within areas of recent geol
- Page 24 and 25: British Geological Survey Research
- Page 26 and 27: Palaeospiroplectammina mellina, End
- Page 28 and 29: PERMIAN 100 DUCKMANTIAN BOLSOVIAN L
- Page 30 and 31: eds. The upper part of the formatio
- Page 32 and 33: British Geological Survey Research
- Page 34 and 35: Thickness Up to 90 m Distribution P
- Page 36 and 37: calcisiltites of the Clitheroe Lime
- Page 38 and 39: Bowland Basin, and to the south-eas
- Page 40 and 41: Raven’s Tor, Dovedale [SK 1412 53
- Page 42 and 43: Reference sections Woo Dale Borehol
- Page 44 and 45: in regional correlation of the succ
- Page 46 and 47: Age Brigantian 4.5.8.1 upper miller
- Page 48 and 49: ing order 6.90, 0.32 and 4.93 m thi
- Page 50 and 51: at the eastern end of an elongate m
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dominated shelf environment (Carney
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Genetic interpretation There are co
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on, and overstepping, Tournaisian l
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PERMIAN MARSDENIAN Depth in metres
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Lower and upper boundaries The base
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Llangollen [SJ 23 45], and near Osw
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Type section The lowermost exposed
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Type section Stream section at Whit
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Limestone in the Middop Anticline (
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Reference sections Composite sectio
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Man, lavas, volcaniclastic debris f
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Age Late Asbian to early Brigantian
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Age Brigantian 4.7.7 Bowland Shale
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Distribution Does not crop out. Pro
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intertonguing with the Cefn-y-fedw
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Thickness From about 200 m at north
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the marine band is absent from the
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Biostratigraphical characterisation
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Thickness About 55 to 215 m Distrib
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WBH Isopachs upon the Rossendale Fo
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ASTURIAN BOLSOVIAN Phillipsi Upper
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is taken at the top of the dark gre
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Age Bolsovian 4.9.3.6 hemsWorth mem
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Age Westphalian 4.10.2 Halesowen Fo
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name for part of the Silurian in th
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Biostratigraphical characterisation
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5 South Wales-Bristol The area sout
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British Geological Survey Research
- Page 108 and 109:
et al., 2002). The undivided Avon G
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Lower and upper boundaries The base
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Genetic interpretation The formatio
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Lithology Dark grey, thin- to mediu
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complex of ooidal barrier shoal (Co
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5.2.14 Oxwich Head Limestone Format
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the Abercriban Oolite Subgroup and
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Lithology Massive, medium-grained,
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Lithology A heterolithic, lenticula
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Regional correlation Same age as, a
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Age Tournaisian 5.2.27 Vallis Limes
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1977). These deposits were subseque
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Type section North side of Cheddar
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the type section of the Kenfig Bore
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Biostratigraphical characterisation
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(Stubblefield and Trotter, 1957), t
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a WARWICKSHIRE GROUP SOUTH WALES CO
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The Subcrenatum Marine Band is not
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Valley, south Wales: exposes 44 m o
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Mangotsfield members, maintaining t
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Reference section Hursley Hill Bore
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litharenite petrography of the sand
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Reference section Steeple Aston Bor
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6 South-west England To the south o
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SOUTH DEVON BASIN TAVY BASIN RUSEY
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laterally into the numerous middle/
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pale to dark grey, massive to plana
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entire member, 7 m thick, is seen t
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Biostratigraphical characterisation
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have been obtained from the ?underl
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formation intertongues with the Buc
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Age ?Famennian to Visean 6.6 CHUDLE
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Thickness Unknown, but a minimum th
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Lithology Thin-bedded mudstones, si
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BriDge, D m, CarNey, J N C, laWley,
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falCoN, N l, and keNt, p e. 1960. G
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lovell, r W W. 1978. The sedimentol
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elations of its older stratified de
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Waters, C N, glover, B W, and poWel
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Supergroup Group Sub-group Formatio
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Supergroup Group Formation Member C
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Group Formation Member Tamar (TAMA)
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Appendix 2 Redundant lithostratigra
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ACH Mount Ararat Chert Formation Co