Petrogenesis and thermal history of the Kunlun batholith, northern Tibet
The Kunlun Terrane is the most northerly of the several microplates that comprise the Tibetan Plateau. Geochronological data from the Kunlun batholith defines three distinct periods of intrusion at 390 Ma, 250 Ma and 190 Ma. A model is presented whereby the Devonian intrusions are considered to be r...
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Open University
1988
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| Online Access: | https://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.233921 |