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## Abstract A recent interpretation of the structural geology and chronology of the northwestern envelope of the Main Donegal Granite by Hutton (1977) is critically examined. Although many aspects of this analysis are sound, there remains serious doubt concerning Hutton's main conclusion that the intense deformation near the granite resulted from its forceful intrusion.

Author

A. R. Berger

Publisher

John Wiley and Sons; Wiley (John Wiley & Sons); John Wiley & Sons Inc.; Wiley (ISSN 0072-1050)

Published

1980

Language

EN