Geochemical and zircon U-Pb-Hf-O isotopic evidence for a coherent Paleoproterozoic basement beneath the Yangtze Block, South China
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文摘

New findings of Paleoproterozoic orthogneisses in the eastern Yangtze Block.

A-type granite protolith for orthogneisses that formed in a post-orogenic setting.

The 1.85 Ga A-type magmatism led to overall craton stabilization in the Yangtze Block.

A coherent Paleoproterozoic basement beneath the Yangtze Block.

The Yangtze Block represents an important part of the Columbia supercontinent.

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