70:. The southern margin of the fault system is defined by the Church Stretton Fault and Dulas Valley Fault, amongst others whilst its northern margin is defined by the Garth-Llanwrtyd Fault Belt in Carmarthenshire. The Church Stretton Fault component of the system is deemed to form the
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Geology of the
Llandovery District - a brief explanation of the geological map sheet 212 ‘Llandovery’
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101:defines the opposing northwestern margin.
155:Geological History of Britain and Ireland
134:The Geological Society, London (pp14-15)
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153:Woodock, N.H.; Strachan, R.A. (2000).
89:and was reactivated during the later
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121:The Geological Society, London (p80)
157:. Blackwell Science. p. 187.
31:which runs northeastwards through
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132:The Geology of England and Wales.
119:The Geology of England and Wales.
85:The system was active during the
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21:Welsh Borderland Fault System
97:within Britain, just as the
16:Fault zone in Great Britain
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78:to its northwest and the
190:Geology of Shropshire
74:boundary between the
61:Pontesford Lineament
55:. It comprises the
82:to its southeast.
87:Caledonian Orogeny
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185:Geology of Wales
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99:Moine Thrust
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179:Categories
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105:References
68:Fault Zone
49:Shropshire
39:through
25:faulting
72:terrane
53:England
29:folding
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95:orogen
47:into
45:Powys
35:from
33:Wales
159:ISBN
63:and
43:and
19:The
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