Clay mineral distribution characteristics of surface sediments in the South Mid-Atlantic Ridge

Hu, Qian-Nan; Li, Chuanshun; Yang, Bojun; Fang, Xisheng; Lu, Hongfeng; Shi, Xuefa; Liu, Jihua

doi:10.1007/s00343-022-2033-1

Cited by 3 publications

(1 citation statement)

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“…However, some REY-rich minerals incorporated in phillipsite aggregates can contribute to the enrichment of REY. Other studies have also focused on the contribution of clay mineral [30,31], Fe/Mn oxyhydroxides [4,32], and Fe/Mn micronodules [33] to the enrichment of REY-rich sediments.…”

Section: Introductionmentioning

confidence: 99%

Grain Size Analyses and Mineral Compositions of Core Sediments in the Western North Pacific Ocean: Implications for the Rare Earth Element and Yttrium Enrichment and Deposition Environment

Hu,

Yu,

et al. 2023

Minerals

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Rare earth element and Yttrium (REY)-rich deep-sea sediments have been identified as significant potential resources. Although grain size analysis is important for the study of deposition environment and the future exploration of REY, related research is limited. Here, we have investigated the grain size and mineral composition of bulk pelagic sediments from Western North Pacific to indicate the evolutions of deposition environment. Grain size analysis results reveal that silt contents are dominant, and the grain size ranges between 20 and 40 μm and can be an additional grain characteristic indicator for REY-rich sediments. Furthermore, the better sorting coefficient of REY-rich sediments reflects the scouring action of bottom currents, which allows the preservation of coarse-grained bioapatite and the removal of clay fraction particles. ΣREY is negatively correlated with clay fractions but positively correlated with sand and silt fractions for the REY-rich sediments, and this is consistent with the dominant distribution of silt-sized biogenic apatite. In addition, grain size distribution (GSD) varies significantly after HCl treatment in the REY-rich sediment. Therefore, for deep-sea sediments collected below the carbonate compensation depth (CCD), an additional presence of a grain size peak at ~20–40 μm and distinct differences in GSD after HCl treatment can serve as important indicators for REY enrichment sediments.

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