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An oxidized and hydrous mantle beneath the Iranian continent since the cretaceous: Insights from the Sanandaj lavas
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DOI：10.1016/j.lithos.2026.108705.png)
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Abstract
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• A suite of Cretaceous basalts and andesites were identified in the northwest Iran. • The oxidized and hydrous mantle beneath Iran was since Cretaceous (127.9 Ma). • The Cretaceous magmatic rocks are potential to form copper deposits.
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