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Surge zones in the Moine thrust zone of NW Scotland


, : Surge zones in the Moine thrust zone of NW Scotland. Journal of Structural Geology 4(3): 247-256

The Caledonian thrust zones of Assynt show several examples of large fault-bounded structures, surge zones, up to 8 km2 in extent, which have moved further than adjacent rocks. Extensional faults can be traced into strike-slip faults and then to contractional imbricate faults. There are also zones of extensional and contractional flow as shown by strained bioturbation marks in the Cambrian Pipe Rock.

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DOI: 10.1016/0191-8141(82)90012-8


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