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164:. The rocks of the Gala Group have also previously been known as the Queensberry Grits and the Strangford Group. Graded beds variously of
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188:. The strata are generally near-vertical and are bounded to the north by the
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and have been matched with the
Central Belt turbidites which are seen in the
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G.J. H. Oliver et al. The
Geological Society (2002). Trewin, N.H. (ed.).
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243:(4. ed.). London: Geological Society Publishing. pp. 187–188.
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192:and to the south by the Laurieston Fault.
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289:Geologic formations of the United Kingdom
284:Geological groups of the United Kingdom
205:
16:Series of rock strata in Great Britain
7:
218:The BGS Lexicon of Named Rock Units
14:
1:
220:. British Geological Survey
156:. The name is derived from
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269:Silurian System of Europe
196:are found in a few beds.
26:
241:The Geology of Scotland
160:, a tributary of the
279:Geology of Scotland
190:Orlock Bridge Fault
176:are interpreted as
57:Orlock Bridge Fault
28:Stratigraphic range
274:Geology of England
135:lithostratigraphic
69:(faulted boundary)
67:Moffat Shale Group
152:and northernmost
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105:Scotland, England
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186:Northern Ireland
146:Southern Uplands
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140:(a sequence of
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182:Ards Peninsula
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222:. Retrieved
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214:"Gala Group"
208:
127:
125:
110:Type section
34:- Telychian
194:Graptolites
162:River Tweed
142:rock strata
263:Categories
200:References
178:turbidites
166:wackestone
158:Gala Water
128:Gala Group
119:Gala Water
91:turbidites
32:Rhuddanian
22:Gala Group
224:August 8,
170:siltstone
144:) in the
115:Named for
82:Lithology
74:Thickness
52:Underlies
174:mudstone
150:Scotland
132:Silurian
97:Location
63:Overlies
36:Silurian
154:England
102:Country
87:Primary
55:bounds
247:
77:c6000m
138:group
130:is a
46:Group
245:ISBN
226:2016
172:and
126:The
42:Type
184:in
148:of
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216:.
168:,
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253:.
228:.
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