Geology of the Ordovician rocks between Leadhills and Abington, Lanarkshire
NE-SW faults in the Abington area of the Northern Belt of the Southern Uplands define blocks up to 3.2 km wide. The strata, folded and locally overturned, young predominantly to the NW but blocks to the SW contain younger sequences. Analogous configurations occur in modern accretionary margins. The...
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University of St Andrews
1981
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| Online Access: | http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.594410 |