Chemical composition of nodules and crusts from the Sea of Japan

Iron-manganese mineralization on seamounts and rises in the Sea of Japan is represented by iron-manganese nodules and crusts. Their chemical composition (major elements and more than 30 trace elements) was studied by a series of analytical methods. According to geochemical comparisons hydrogenic, hydrothermal, and biogenic materials have participated in creation of this mineralization. Contents of Ba and Li, as well as Mo/Pb and Sb/As ratios can be used as indicators of genesis of iron-manganese nodules and crusts along with composition of the rare earth elements.

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Cite this as

Baturin, Gleb N (1990). Dataset: Chemical composition of nodules and crusts from the Sea of Japan. https://doi.org/10.1594/PANGAEA.758855

DOI retrieved: 1990

Additional Info

Field Value
Imported on November 30, 2024
Last update November 30, 2024
License CC-BY-3.0
Source https://doi.org/10.1594/PANGAEA.758855
Author Baturin, Gleb N
Given Name Gleb N
Family Name Baturin
Source Creation 1990
Publication Year 1990
Resource Type application/zip - filename: Baturin_1990
Subject Areas
Name: Oceans

Related Identifiers
Title: The geochemistry of iron-manganese formations on the Sea of Japan floor
Type: DOI
Relation: IsSupplementTo
Year: 1990
Source: Oceanology
Authors: Baturin Gleb N .