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Jefferies, Sharon P.
The Median Tectonic Line (MTL) is a major, crustal-scale fault in Japan that separates the low-P/high-T Ryoke metamorphic belt of mainly subduction related granitoids from the high-P/low-T Sambagawa Belt of accretionary complex metasedimentary rocks.
Externí odkaz:
http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.550024
