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The nature (i.e., sub‐oceanic, sub‐arc or sub‐continental) of ophiolitic mantle peridotites from the eastern Neo‐Tethyan domain in southern Tibet has been hotly debated. This uncertainty limits our understanding of the history and evolution of the eastern Neo‐Tethys Ocean. Here we present petrological, geochemical and Re‐Os isotopic data for the mantle peridotites from the Dazhuqu ophiolite in the...
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