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- W4387079180 abstract "Mineral magnetic and geochemical investigations were carried out on a short sediment core collected from the eastern Southwest Indian Ridge (ESWIR) to study the variations in the source components. The magnetic concentration parameter χarm represents the concentration of single stable domain (SSD) sized grains, χarm/χlf, χarm/SIRM are magnetic grain size ratios and the geochemical ratios Fe/Ti, Co/Zn, and Zn/Fe and Ba content serve as hydrothermal indicators, all of which show a distinct top - bottom variability. The magnetomineralogical parameters S-ratio and coercivity (Hc) also follow these variations suggesting an increased contribution from hydrothermal components in the top 15 cm of the core. Significant enrichments of Fe, Mn, and Mg in the samples, along with depletions of detrital elements Al, Si, Rb, Zr, Hf, and Nb in the element/Upper Continental Crust (UCC) values, show that the majority of the detrital component is locally sourced. Thermomagnetic measurements of samples indicate that the major remanence carrier is magnetite in the core, along with minor contributions from titanomagnetite, hematite, and iron sulfides." @default.
- W4387079180 created "2023-09-28" @default.
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- W4387079180 date "2023-11-01" @default.
- W4387079180 modified "2023-10-09" @default.
- W4387079180 title "Unmixing the hydrothermal and detrital components from a metalliferous sediment core from the eastern southwest indian ridge – Insights from mineral magnetism" @default.
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- W4387079180 doi "https://doi.org/10.1016/j.dsr.2023.104162" @default.
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