Zircon ages and Hf isotopic compositions of Ordovician and Carboniferous granitoids from central Inner Mongolia and their significance for early and late Paleozoic evolution of the Central Asian Orogenic Belt
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文摘

New zircon ages and Hf isotopic compositions for plutonic rocks.

Early and late Paleozoic evolution of the Central Asian Orogenic Belt.

Ordovician granitoids represent adakitic granitoids.

Carboniferous granitoids are typical subduction-related arc granitoids.

CAOB evolved through several subduction systems with different polarities.

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