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Reply to “Constraints on the significance of the Orlock Bridge Fault within the Scottish Southern Uplands”, a discussion of “The Orlock Bridge Fault: a major Late Caledonian sinistral fault in the Southern Uplands terrane, British Isles”

Published online by Cambridge University Press:  03 November 2011

T. B. Anderson  and
G. J. H. Oliver
T. B. Anderson
Affiliation:
Department of Geology, The Queen's University of Belfast, Belfast BT7 1NN, Northern Ireland.
G. J. H. Oliver
Affiliation:
Department of Geology, University of St Andrews, St Andrews KY16 9ST, Scotland.
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Extract

We naturally regret our failure to convince the British Geological Survey's Southern Uplands team of the nature and importance of the fault which separates Northern and Central Belts, two of the three fundamental divisions of the Southern Uplands terrane which were so brilliantly recognised and defined by their illustrious predecessors (Peach & Home 1899). We welcome the opportunity to clarify the basis of our argument and correct some quite erroneous impressions.

Type
Reply
Information
Earth and Environmental Science Transactions of The Royal Society of Edinburgh , Volume 78 , Issue 3 , 1987 , pp. 223 - 225
Copyright
Copyright © Royal Society of Edinburgh 1987

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References

Anderson, T. B. & Oliver, G. J. H. 1986. The Orlock Bridge Fault: a major Late Caledonian sinistral fault in the Southern Uplands terrane, British Isles. TRANS R SOC EDINBURGH: EARTH SCI 77, 203–222.CrossRefGoogle Scholar
Barnes, R. P., Anderson, T. B. & McCurry, J. A. 1987. Along-strike variation in the stratigraphical and structural profile of the Southern Uplands Central Belt in Galloway and Down. J GEOL SOC LONDON 144, 807–816.CrossRefGoogle Scholar
Cameron, T. D. J. & Anderson, T. B. 1980. Silurian metabentonites in County Down, Northern Ireland. GEOL J 15, 59–75.CrossRefGoogle Scholar
Craig, L. E. 1984. Stratigraphy in an accretionary prism: the Ordovician rocks in North Down, Ireland. TRANS R SOC EDINBURGH EARTH SCI 74, 183–191.CrossRefGoogle Scholar
Davies, A., McAdam, A. D. & Cameron, I. B. 1986. Geology of the Dunbar district. MEM GEOL SURV SCOTLAND, Sheet 33(E) and part of Sheet 41.Google Scholar
Floyd, J. D., Stone, P., Barnes, R. P. & Lintern, B. C. 1987. Constraints on the significance of the Orlock Bridge Fault within the Scottish Southern Uplands. TRANS R SOC EDINBURGH: EARTH SCI 78, 219–221.CrossRefGoogle Scholar
Griffith, A. E. & Wilson, H. E. 1982. Geology of the country around Carrickfergus and Bangor. MEM GEOL SURV NORTH IREL, Sheet 29.Google Scholar
Kelling, G. 1961. The stratigraphy and structure of the Ordovician rocks of the Rhinns of Galloway. J GEOL SOC LONDON 117, 37–75.CrossRefGoogle Scholar
Leggett, J. K., McKerrow, W. S. & Eales, M. H. 1979. The Southern Uplands of Scotland: a Lower Palaeozoic accretionary prism. J GEOL SOC LONDON 136, 755–70.Google Scholar
McAdam, A. D. & Tulloch, W. 1985. Geology of the Haddington district. MEM GEOL SURV SCOTLAND, Sheet 33(W) and part of Sheet 41.Google Scholar
Peach, B. N. & Horne, J. 1899. The Silurian rocks of Britain, 1, Scotland. MEM GEOL SURV SCOTLAND.Google Scholar
Simpson, C. & Schmid, S. M. 1983. An evaluation of criteria to deduce the sense of movement in sheared rocks. BULL GEOL SOC AM 94, 1281–88.2.0.CO;2>CrossRefGoogle Scholar
Strachan, I. 1982. The distribution of graptolites in south-east Scotland, with notes on the fauna of Old Cambus Quarry. SCOTT J GEOL 18, 157–165.CrossRefGoogle Scholar