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Ordovician-Late Silurian geodynamics of north Queensland

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posted on 2016-08-30, 09:43 authored by Robin ArmitRobin Armit, Peter BettsPeter Betts, JOHN STEWARTJOHN STEWART
Palaeozoic continental growth and accretionary tectonism along the eastern margin of Gondwana is characterised by the inversion of back-arc basins and accretion of the magmatic arc terranes and micro-continental ribbons.

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    Monash Structural Geophysics Group

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    tasmanidesGondwana supercontinentImagingLocusGeologyGeophysicsTectonicsSolid Earth Sciences

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