Garnfor Intrusion

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Journal Article
Published: 01 August 1991
Journal of the Geological Society (1991) 148 (4): 703–710.
... that agree with the generally accepted view that the rocks are of Ordovician age. These rocks have fairly consistent initial ratios within the range 0.7045 f 0.0010 (2a) which is taken as representing the Sr-isotopic composition of the magma at the time of intrusion. Inner Garnfor (Fig. 20) is included...