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Thermochronological constraints on the late Paleozoic tectonic evolution of the southern Chinese Altai
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文摘

40Ar/39Ar amphibole ages are consistently at ∼270 Ma along the southern Chinese Altai.

40Ar/39Ar biotite ages are variable from 264 to 226 along the southern Chinese Altai.

40Ar/39Ar ages constrain the cooling process of the southern Chinese Altai.

The cooling process was possibly related to the development of the Erqis Shear Zone.

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