Distribution, chronology and causes of Cretaceous - Cenozoic magmatism along the magma-poor rifted southern Australian margin: Links between mantle melting and basin formation
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The magma-poor Australian margin hosts many yet undescribed igneous features.

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Offshore magmatism is younger than any break-up events along the margin.

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Offshore magmatism does not fit with onshore magmatic age-trends.

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No evidence was found for plume activity causing the offshore magmatism.

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Clear links exist between Tasmanian magmatism and basin evolution in the bass basin.

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