Validating models of channel flow, ductile extrusion and exhumation : the Greater Himalayan Sequence, Annapurna Massif
Himalayan orogenesis is commonly explained with models of channel flow, in which the metamorphic core, referred to as the Greater Himalayan Sequence (GHS), forms a partially molten, rheologically weak mid-crustal flow. Geochronological and thermobarometric studies from the Himalaya provide support f...
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University of Leeds
2015
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| Online Access: | http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.655276 |