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| quote: | | Fleurieu Penisula (Ludbrook, 1980), is where Precambrian and Early Cambrian rock sequences in eastern Australia experienced Cambrian deformation and metamorphism. The orogeny extends through South Australia (South Australian Adelaide fold belt), Victoria (Glenelg fold belt), New South Wales (Wonaminta block) and even into Tasmania (Precambrian and Cambrian sequences) (Foden et al. 2006). The orogeny and belts associated are a result of the consequence of stress transfer to the outer trailing edge of the newly forming continent at that time, Gondwana. The Delamerian, by definition, is therefore a compressional orogenic zone with westward-verging folds and thrust faults (Foden et al. 2006). |
lol. 1st year geology 
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