Mesozoic-Tertiary sedimentary and tectonic evolution of the South-Tethyan continental margin and Late Cretaceous ophiolite in Baer-Bassit region (N.W. Syria)
The Baer-Bassit area of NW Syria exemplifies the evolution of Neotethys at the W end of the "ophiolitic crescent". The stratigraphy of the Baer-Bassit area is divisible into four main units. 1) At the base, there is a relatively autochthonous Mesozoic Arabian carbonate platform (1500-1800...
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University of Edinburgh
2000
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| Online Access: | http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.640319 |