Late Ordovician back-arc extension in the southeastern margin of the Tarim Craton, NW China: Elemental and Sr-Nd isotopic constraints from the Hongliugou basalts | Zendy

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Late Ordovician back-arc extension in the southeastern margin of the Tarim Craton, NW China: Elemental and Sr-Nd isotopic constraints from the Hongliugou basalts

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