Geochronology and geochemistry of the Triassic bimodal volcanic rocks and coeval A-type granites of the Olzit area, Middle Mongolia: Implications for the tectonic evolution of Mongol-Okhotsk Ocean
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文摘

Late Triassic age for the Olzit bimodal suite and coeval granites.

Basaltic end-member derived from partial melting of an enriched lithospheric mantle.

Granites and rhyolitic end-member of the bimodal suite have A-type affinity.

Olzit bimodal suite and coeval granites represent a back-arc basin extension of the Mongol–Okhotsk Ocean.

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