In the underground workings, dispersed ridge-in-groove lineations and striations on the vein walls suggest oblique dextral shearing on the NNE-striking quartz veins, but almost pure left-lateral shearing on the NeS fault planes. The NNW-trending quartz veins occur in zones where dikes are ...
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In Proceedings of the Fifth International Conference on Basement Tectonics, Cairo, Egypt, 16–18 October 1983; International Basement Tectonics Association: Oak Ridge, TN, USA, 1983. [Google Scholar] Khudeir, A.A.; El-Gaby, S.; Kamal El Din, G.M.; Asran, A.M.; Greiling, R.O. The...