Glaciomarine model for upper Precambrian diamictites of the Port Askaig Formation, Scotland

Descriptive techniques (lithofacies codes) and vertical profile analysis emphasizing lithofacies contacts and geometry allow objective characterization and comparison of diamict(ite) sequences irrespective of geologic age. Upper Precambrian diamictites (?650−600 m.y.) of the Middle Dalradian Port Askaig Formation in Scotland are traditionally interpreted as products of repeated ice-sheet advances over an emergent shallow marine shelf and …