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This article focuses on the Cretaceous structures in the Duolong region, northern Tibet. Our aim was to constrain the metallogenic setting of the Duolong giant porphyry Cu–Au deposit and to discuss the implications for the closure of the Bangong–Nujiang Neo-Tethys Ocean. There are two tectonic stages in the Duolong region, during the Early to Late Cretaceous. The first stage is characterised by numerous...
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