Emplacement of sub-volcanic cone sheet intrusions
Sub-volcanic intrusive networks, of which cone sheets are recognised as a major constituent, control volcano growth and eruption style. The accepted cone sheet model is that these confocally dipping intrusions originate from an unexposed central magma chamber through dip-parallel magma flow. However...
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University of Birmingham
2011
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| Online Access: | https://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.542121 |