Origin of the New England contorted mountain belt: implications for plate tectonics, magmatism and mineralisation

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The southern New England mountain chain in eastern Australia is characterised by a tight curved geometry. This research will reconstruct the formation of these, hitherto unexplained, mountain curves, unravelling their driving mechanisms and tectonic processes. Results will provide a plate tectonic model for the formation of economic resources, thus facilitating future discoveries of ore deposits in the New England belt, or energy resources in the associated sedimentary basins. The project will foster a pool of highly trained professionals and researchers in the fields of structural geology and tectonics, and will enhance Australia's scientific reputation, maintaining its leading international standing in plate tectonic research.