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author Stoffers, Peter
Sioulas, A
Glasby, Geoffrey P
Thijssen, Theo
author_facet Stoffers, Peter
Sioulas, A
Glasby, Geoffrey P
Thijssen, Theo
collection Datos científicos de ciencias marinas y ambientales
contents Inside core 710KH, manganese micronodules are much more abundant in the coarse fraction (> 40 μm) of the dark brown clay horizon than in the upper sedimentary unit and are characterized by higher ratios and higher Ni and Cu contents than those from the upper-sediment horizon. This reflects the fact that these "overconsolidated" sediments are well oxidized and that element remobilization from the micronodules has not taken place within this sediment type. In the upper sedimentary unit there is a sharp drop in the ratio and Ni and Cu contents of the micronodules immediately beneath the sediment surface, reflecting the selective migration of Mn and other transition elements such as Ni and Cu from the micronodules.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_960141
institution PANGAEA
language en
publishDate 2023
publisher PANGAEA
record_format pangaea
spellingShingle Chemical composition of manganese micronodules at various depths in core 710KH from campaign SO11 of R/V Sonne
Stoffers, Peter
Sioulas, A
Glasby, Geoffrey P
Thijssen, Theo
Aluminium oxide; Barium; BC; Box corer; Cobalt; Copper; Deposit type; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Elevation of event; Event label; Geochemistry; Grain size, maximum; Grain size, mean; Grain size, minimum; Identification; Iron; Latitude of event; Lead; Longitude of event; Manganese; manganese nodule; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; ocean; Peru Basin, Pacific Ocean; Sediment type; Silicon dioxide; SO11; SO11_710KH; Sonne; SOPAC II; Titanium; Wet chemistry; Zinc
Inside core 710KH, manganese micronodules are much more abundant in the coarse fraction (> 40 μm) of the dark brown clay horizon than in the upper sedimentary unit and are characterized by higher ratios and higher Ni and Cu contents than those from the upper-sediment horizon. This reflects the fact that these "overconsolidated" sediments are well oxidized and that element remobilization from the micronodules has not taken place within this sediment type. In the upper sedimentary unit there is a sharp drop in the ratio and Ni and Cu contents of the micronodules immediately beneath the sediment surface, reflecting the selective migration of Mn and other transition elements such as Ni and Cu from the micronodules.
title Chemical composition of manganese micronodules at various depths in core 710KH from campaign SO11 of R/V Sonne
topic Aluminium oxide; Barium; BC; Box corer; Cobalt; Copper; Deposit type; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Elevation of event; Event label; Geochemistry; Grain size, maximum; Grain size, mean; Grain size, minimum; Identification; Iron; Latitude of event; Lead; Longitude of event; Manganese; manganese nodule; Nickel; NOAA and MMS Marine Minerals Geochemical Database; NOAA-MMS; ocean; Peru Basin, Pacific Ocean; Sediment type; Silicon dioxide; SO11; SO11_710KH; Sonne; SOPAC II; Titanium; Wet chemistry; Zinc
url https://doi.org/10.1594/PANGAEA.960141