Magma-cryosphere interactions on Mars : the influence of heat-transfer mechanisms on surface morphology
Mars is thought to have a planet-wide cryosphere of several kilometres depth consisting of a mixture of rock and permanently frozen ice. The physical processes occurring during magma-cryosphere interaction (MCI) appear to have played a large part in the morphological development of many regions of M...
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Lancaster University
2016
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| Online Access: | http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.727389 |