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U-Pb geochronology and geochemistry of Bibi-Maryam pluton, eastern Iran: Implication for the late stage of the tectonic evolution of the Sistan Ocean
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文摘

The closure of the Sistan Ocean (one of Neo-Tethyan branch) postdates the Paleocene.

Adakites in eastern Iran could be formed in an intra-oceanic subduction system.

Genesis of adakites via slab melting has been discussed.

We reported new age for magmatism in eastern Iran.

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