Yong, C. K.2019-07-052019-07-051964http://hdl.handle.net/2440/119915This item is only available electronically.The area of uniform stratigraphic sequence studied is essentially part of the west limb of a regional anticlinorium. Both the mesoscopic and the macroscopic folds have the same concentric style. Two different explanations are suggested for the apparently odd occurrence of a 30-foot arkosic quartzite band near the top of the northern foothills.enHonours; Geology; Adelaide Geosyncline; Adelaidean; stratigraphy; structureThesis