The Ross Orogen of the Transantarctic Mountains

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Focusing on the geological evolution of the Ross orogen, this book details its formation from the Neoproterozoic through the early Paleozoic, highlighting significant tectonic events and the culmination of the Ross orogeny around 500 million years ago. It synthesizes classical studies with contemporary research, including controversial theories regarding the rifting of Laurentia from Gondwanaland. Additionally, it features a comprehensive bibliography and a historical timeline of expeditions, making it an essential resource for geologists and researchers interested in Antarctic geology.