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Miocene depositional environment and climate in western Europe: The lignite deposits of the Lower Rhine Basin, Germany
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文摘

Lignites were analyzed using geochemical, micropetrographical and isotope analysis.

A modified groundwater index is introduced based on ash content and micropetrography.

Strong pore water exchange influenced peat/lignite composition.

Temperatures based on GDGTs reveal a cooling trend initiated in the Upper Miocene.

Isotopic trends support angiosperm-dominated flora and changing climate.

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