Introduction to 'Comparison between intracratonic and active margin basins: Examples from the Late Paleozoic of western Gondwana'

摘要

Western Gondwana basins are key to understanding the evolution of the Gondwana supercontinent during the Late Paleozoic. The western margin of Gondwana underwent a complex tectonic history with continuous paleogeographic changes, including the formation of orogenic belts and basins, as discussed by Lopez Gamundi et al. (1994) and Vee-vers and Powell (1994) in "Permian-Triassic Pangea Basins and Fold belts along the Panthalassan Margin of Gondw-analand."