Early Permian Sunidyouqi suprasubduction-zone ophiolites in the central Solonker suture zone (Inner

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Different final closing ages have been proposed for the evolution of the Paleo-Asian Ocean (PAO), including Late Silurian, pre-Late Devonian, Early Permian, Late-Permian and Late PermianeEarly Triassic. Ophiolites represent fragments of ancient oceanic cr
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