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sequence are parallel, so little rotational movement occurred during the first stage. The second stage of movement happened in the middle-to-late
Jurassic period, when strong rotation happened, up to 24 degrees.
56:. In the offshore area it is a major normal fault and forms the bounding structure to the Cardigan Bay Basin, with a fill including about 2,500 metres (8,200 ft) of
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The fault is believed to have experienced two separate stages of movement. The horizons between the upper
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Modeling The Earth For Oil
Exploration: Final Report of the CEC's Geoscience I
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View south-west along the fault line with
Talyllyn Lake in the valley bottom
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This article about a specific United
Kingdom geological feature is a
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76:. At its northeastern end it links to the similarly orientated
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127:(2 ed.). Geological Society. p. 339.
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121:Brenchley, P.J.; Rawson, P.F. (2006).
60:. Onshore, it is responsible for the
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287:. You can help Knowledge (XXG) by
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102:List of geological faults of Wales
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279:This article about a location in
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124:The geology of England and Wales
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161:. Elsevier. pp. 249–.
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18:Bala - Llanelidan Fault
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138:. Retrieved
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140:8 December
108:References
58:Lias Group
42:Bala Fault
62:lineament
96:See also
89:Jurassic
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188:4°04′W
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