Fig. 2: Discrimination of nodule genesis using high field strength elements and rare earth elements. | Communications Earth & Environment

Fig. 2: Discrimination of nodule genesis using high field strength elements and rare earth elements.

From: Molybdenum isotope fractionations between ferromanganese oxides and seawater influenced ancient sedimentary isotopic signatures

Fig. 2: Discrimination of nodule genesis using high field strength elements and rare earth elements.The alternative text for this image may have been generated using AI.

a, b using metal element indicator34; c, d using rare earth elements and Y indicator33. The Ce anomaly (Ce/Ce*) is calculated using the equation Ce/Ce* = Cen/(Prn2/Ndn), where n denotes normalization of each concentration against the post-Archean Australian shale (PAAS)51.

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