Rare earth elements in bottom sediments from the deeps of the Red Sea rift zone

DOI

Analysis of rare earth element (REE) distribution and behavior in ore-bearing hydrothermal-sedimentary deposits from the Red Sea is carried out. Geochemical patterns and mechanisms of REE accumulation in metalliferous sediments of the open ocean and in deposits adjoined to areas of hydrothermal discharge are shown. Main factors, which determine composition of REE and the level of their accumulation in hydrothermal occurrences of the Red Sea, are considered.

Supplement to: Butuzova, Galina Yu; Lyapunov, Sergey M (1995): Rare earth elements in hydrothermal-sedimentary deposits from the Red Sea. Translated from: Litologiya i Poleznyye Iskopaemyye, 1995, 1, 16-30, Lithology and Mineral Resources, N 1, 13-26

Identifier
DOI https://doi.org/10.1594/PANGAEA.774363
Related Identifier IsSupplementTo https://doi.org/10.1016/j.gr.2014.10.008
Metadata Access https://ws.pangaea.de/oai/provider?verb=GetRecord&metadataPrefix=datacite4&identifier=oai:pangaea.de:doi:10.1594/PANGAEA.774363
Provenance
Creator Butuzova, Galina Yu; Lyapunov, Sergey M
Publisher PANGAEA
Contributor Geological Institute, Russian Academy of Sciences, Moscow
Publication Year 1995
Rights Creative Commons Attribution 3.0 Unported; https://creativecommons.org/licenses/by/3.0/
OpenAccess true
Representation
Resource Type Supplementary Publication Series of Datasets; Collection
Format application/zip
Size 5 datasets
Discipline Earth System Research
Spatial Coverage (37.583W, 17.888S, 39.813E, 22.785N); Red Sea; Red Sea, Tethis Deep; Red Sea, Atlantis II Deep; Red Sea, Shagara Deep