- Page 1: A lithostratigraphical framework fo
- Page 6 and 7: BRiTisH GeoloGiCAl suRvey The full
- Page 8 and 9: Acknowledgments This report is the
- Page 10 and 11: TABLES 1 Chronostratigraphical fram
- Page 12 and 13: British Geological Survey Research
- Page 14 and 15: a mudstone-dominated succession cha
- Page 16 and 17: Uplands 60°N 5°W 0° 5°W 0° 5°
- Page 18 and 19: Table 1 Chronostratigraphical frame
- Page 20 and 21: Table 2 Tournaisian and visean bios
- Page 22 and 23: Table 4 westphalian chronostratigra
- Page 24 and 25: Principal lithofacies Volcanic lith
- Page 26 and 27: 4 Carboniferous rocks of scotland n
- Page 28 and 29: 4 MIDLAND VALLEY OF SCOTLAND 1 3 2
- Page 30 and 31: (or series), which referred, inform
- Page 32 and 33: association of the Ballagan Formati
- Page 34 and 35: Formation by the presence of thicke
- Page 36 and 37: are mostly hypersthene-normative wi
- Page 38 and 39: Lower and upper boundaries Along th
- Page 40 and 41: tic sedimentary rocks to grey plagi
- Page 42 and 43: Distribution and regional correlati
- Page 44 and 45: erosion of the pyroclastic deposits
- Page 46 and 47: lacustrine mudstones containing fos
- Page 48 and 49: section penetrated the middle and b
- Page 50 and 51: Distribution and regional correlati
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The lower north Campsie lavas are g
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Age mid visean (Arundian to Asbian)
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characterised by the presence of va
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1980). The lavas were thought by Cr
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Lithology The skiddaw lava member c
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1970). A reference section is 0.5 k
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there are three massive to variably
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and limestones. To the north of Gla
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Genetic interpretation The pattern
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Lithology The Arthur’s seat volca
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such as the Barracks limestone with
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Stratotype The type area is east lo
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Lower and upper boundaries The base
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Naiadites and Curvirimula, occur in
- Page 80 and 81:
Calmy limestone. The gastropods Mee
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Genetic interpretation Fluviodeltai
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5 Carboniferous rocks of the southe
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Lower and upper boundaries The base
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Age and biostratigraphical characte
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Age and biostratigraphical characte
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12 NORTHEAST NORTHUMBERLAND GL PENN
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Thickness About 170 m seen. Distrib
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deposition on the Askrigg Block occ
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west Cumbria the conglomerates of t
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6.4.4 Stone Gill Limestone Formatio
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Lithology The formation comprises r
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The top of the member has a gradati
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lower Antiquatonia Band to the base
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The Askrigg Block includes the Tom
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millward et al., 2003, fig. 7). str
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6.6.7 Ashfell Limestone Formation (
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8016] from about 143 to 200 m depth
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Distribution and regional correlati
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Age and biostratigraphical characte
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of dark grey limestone above the pa
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various fossil-rich beds (for examp
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unfossiliferous, though some are bu
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terminated and conformably overlain
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marine Bands of the midland valley
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1 BERWICK UPON TWEED AND NORHAM YOR
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WARWICKSHIRE GROUP PENNINE COAL MEA
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1 ROOKHOPE BOREHOLE NORTHERN ENGLAN
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(1932); eastwood et al. (1968); Joh
- Page 138 and 139:
Thickness Between 7 and 10 m north
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Registration Number Ny81sw/7) [Ny 8
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et al., 2001; dickson et al., 1987)
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6.9 MILLSTONE GRIT GROUP (MG) The n
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ase of the mirk Fell ironstones in
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Lingula-band at the base, overlying
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The pennine Coal measures Group (fl
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common at the bases of cyclothems a
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Lower and upper boundaries The base
- Page 156 and 157:
of the underlying pennine Coal meas
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BriTisH geologiCal survey. 2005. ir
- Page 160 and 161:
Museum of Practical Geology for the
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luMsDen, g i, and wilson, r B. 1961
- Page 164 and 165:
siMPson, J B, and MaCgregor, a g. 1
- Page 166 and 167:
Appendix 1 Alphabetical listing of
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Supergroup Group Formation Member N
- Page 170 and 171:
Supergroup Group Formation Member N
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LKL lickar lst LLLM l little lst LM
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Coal measures Group pennine Coal me
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orroland Formation orroland member,