volume 14, issue 4, P362-362 1978
DOI: 10.1144/sjg14040362
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N. J. Soper,
P. E. Brown,
I. W. Fergusson

Abstract: The evidence presented by Fergusson (1978) indicates that the Vagastie Bridge granite post-dates all the main structural and dynamothermal metamorphic events that affected the host Moine rocks. This conclusion, which differs from the statement to the contrary by Dr. Soper and Professor Brown, is based on the evidence at Vagastie Bridge and not on regional correlations. Moreover it is supported not only by the zircon U-Pb age of 405 ±11 Ma given by Pidgeon and Aftalion (1978, p. 190), an age that generally corr…

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