Estimating the impact of early diagenesis on isotope records in shallow-marine carbonates: A case study from the Urgonian Platform in western Swiss Jura
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文摘

Two generations of blocky calcite cements relate to meteoric eogenesis.

Meteoric eogenesis altered whole-rock δ13C up to 45 m below the top karst surface.

The amount and isotope composition of meteoric cements impact the whole-rock δ13C.

Meteoric eogenesis hampers long-distance chemostratigraphic correlation.

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