The Australide orogen, the southern hemisphere Neoproterozoic to Mesozoic terrane accretionary orogen that forms the palaeo-Pacific margin of Gondwana, is one of the largest and longest-lived orogens on Earth. This book brings together a series of reviews and multidisciplinary research papers that comprehensively cover the Australides from the Tasman orogen of eastern Australia to the Neoproterozoic and Palaeozoic orogens of South America, taking in New Zealand and Antarctica along the way. It deals with the evolution of the southern Gondwana margin, as it grew during a series of terrane accretion episodes from the late Proterozoic through to final fragmentation in mid-Cretaceous times. Global perspectives are given by comparison with the Palaeozoic northern Gondwana margin and documentation of world-wide terrane accretion episodes in the Late Triassic-Early Jurassic and mid-Cretaceous. The Tasmanides of eastern Australia, and the terrane histories of New Zealand and southern South America are given comprehensive up-to-date reviews.Structural data for dykes and a shear zone that cut granitoids of the Ford Ranges. ... (a) Southern Ford Ranges stereoplot and rose diagram; (b) northern Ford Ranges stereoplot and rose diagram, exclusive of Fosdick migmatite gneiss domeanbsp;...
|Title||:||Terrane Processes at the Margins of Gondwana|
|Author||:||Alan Vaughan, Philip T. Leat, Robert J. Pankhurst|
|Publisher||:||Geological Society of London - 2005-01-01|