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https://doi.org/10.1144/sjg06010075
Copy DOIJournal: Scottish Journal of Geology | Publication Date: Feb 1, 1970 |
Citations: 12 |
Synopsis Cordierite-bearing xenolithic rocks, including quartz-cordierite-norites, which occur in association with basic igneous rocks in many parts of north-east Scotland, represent Dalradian country rocks which have undergone partial melting at the time of intrusion of the basic magma.
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