Rb—Sr Isotope Age of the Shangdaheyan Intrusion in the Bogda Shan Region and Its Geological Implicat

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The Bogda Shan orogenic belt is interpreted to be an Upper Palaeozoic continental rift,which was closed towards the end of the Carboniferous period,Intrusive activities in that belt are represented mainly by a large number of diabasic sills,dykes and stoc
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