The structure of the Moine‐like rocks near Lough Derg, County Donegal, Eire

摘要

AbstractThe Moine‐like rocks are shown to have major, southward‐leaning, isoclinal F2folds which may be synchronous with the nappe‐like Ballybofey Antiform of the overlying Dalradian rocks. The deformation of the immediately adjacent Dalradian rocks is consistent with a previous suggestion that they are in contact with the Moine‐like rocks along a major tectoni