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Using Mg isotope ratios to trace Cenozoic weathering changes: A case study from the Chinese Loess Plateau
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文摘

The Mg isotopic composition of the Luochuan loess–paleosol sequence is measured.

All samples are isotopically lighter than the UCC.

Shifts in 未26Mg are controlled by changes in carbonate preservation.

Loess sediments cannot be used to estimate the Mg isotopic composition of the UCC.

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