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The Zanhuang domain in the hinterland of the North China Craton, consists of Archaean, Paleoproterozoic, Mesoproterozoic and Palaeozoic rocks, and was previously considered a Mesozoic metamorphic core complex. Our reappraisal of regional structural history and mineral 40 Ar/ 39 Ar geochronology shows that the domain was subjected to a number of deformation events and had...
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