Tectonic evolution of the Bayankhongor Ophiolite, Central Mongolia : implications for the Palaeozoic crustal growth of Central Asia
The Bayankhongor ophiolite marks the closure of an ocean separating two microcontinents: the Baidrag complex with the Burd Gol accretionary complex to the south, and a northern continent which forms the basement for the Hangai region. Subduction was towards the SW with NE-directed ophiolite obductio...
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University of Leicester
2001
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| Online Access: | http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.696988 |