Reply to the discussion by Tanner on 'The Highland Boundary Fault and the Highland Border Complex' Bluck (2010) Scottish Journal of Geology, 46, 113-124

摘要

This is presented in Bluck (2010) fig. 4 where clasts of the rocks to the SE, which are made of tuffs, pillow lavas and cherts, occur in a conglomerate immediately overlying them to the NW. Clasts of chert and lava are also found in the basal parts of the quartzarenite sequence immediately to the NW.