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Sedimentary records of the Neoproterozoic-Cambrian transition on the North China Craton: Chronostratigraphy and provenance of the Huoshan Formation
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DOI：10.1016/j.precamres.2026.108112.png)
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Abstract
En 中文
• Quartz-rich Huoshan Formation forms a compositionally mature unit on the Great Unconformity surface. • The unit records pre-transgressive erosion and sediment recycling on the North China Craton. • Detrital zircon U-Pb ages (n = 696) constrain a Neoproterozoic maximum depositional age and provenance.
Keywords:
Huoshan Formation
Neoproterozoic-Cambrian transition
detrital zircon U-Pb dating
provenance
Great Unconformity
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