Zircon U-Pb and Lu-Hf isotopic and whole-rock geochemical constraints on the Lanhe and Heichashan Groups: Implications for the Paleoproterozoic tectonic basin evolution of the Lüliang Complex
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文摘

The Lanhe Group mostly sourced from the Lüliang Paleoproterozoic rocks.

Most clastics of the Heichashan Group recycled from the underlying Jiehekou Group.

The Heichashan Group deposited at 1.84–1.80 Ga.

2.1 Ga back-arc basin transformed to 1.84–1.80 Ga foreland basin.

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