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Ophiolites represent on‐land fragments of paleo‐oceanic crust and have been recognized as one of the key markers of suture zones. Here, we provide new insights into the emplacement of ophiolitic mélanges based on detailed geological mapping and structural analysis in the West Junggar and Songpan‐Ganzi‐Bayan Har orogens (Fig.1 and Fig.2). The results show that some ophiolitic mélange belts cannot be...
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