Trace element distribution in Neoproterozoic carbonates as palaeoenvironmental indicator

2008/11/07 by Hartwig E. Frimmel · 445 citations
Chemistry · Earth and Planetary Sciences · #Carbonate #Chemistry #Environmental chemistry #Geochemistry #Geochemistry and Elemental Analysis #Geological and Geochemical Analysis #Geology #Hydrothermal circulation #Mineralogy #Oil shale #Paleontology #Paleontology and Stratigraphy of Fossils #Rare earth #Rare-earth element #Sediment #Sedimentary depositional environment #Sedimentary rock #Total organic carbon #Trace element

paper · doi:10.1016/j.chemgeo.2008.10.033

published in Chemical Geology 258(3-4), 338-353 (Elsevier BV)

openalex publication_date 2008/11/07 · openalex created_date 2025/10/10 · openalex updated_date 2026/07/29

Citations

• Has the REE composition of seawater changed over geological time?
• Rare-earth element mobility during hydrothermal and metamorphic fluid-rock interaction and the significance of the oxidation state of europium

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