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The REE species and their distribution in ferromanganese crusts in the Sea of Japan

N. V. Astakhova and V. V. Sattarova
The REE species and their distribution in ferromanganese crusts in the Sea of Japan
Russian Geology and Geophysics (July 2012) 53 (7): 649-656

Abstract

Polished sections of ferromanganese crusts on underwater rises in the Sea of Japan were studied with a JXA8100 microprobe analyser. Mineral phases of REE have been detected. They have Ln (sub 2) O (sub 3) chemical composition, where Ln is La-Ce-Pr-Nd, La-Ce-Nd, or, much more rarely, La-Ce and La-Ce-Pr. With regard to the same chemical composition of REE grains in the ore crusts and basalts from Medvedev Volcano, it has been concluded that these REE were supplied during postvolcanic gas-hydrothermal processes.


ISSN: 1068-7971
Serial Title: Russian Geology and Geophysics
Serial Volume: 53
Serial Issue: 7
Title: The REE species and their distribution in ferromanganese crusts in the Sea of Japan
Affiliation: Russian Academy of Sciences, Pacific Oceanological Institute, Vladivostok, Russian Federation
Pages: 649-656
Published: 201207
Text Language: English
Publisher: Allerton Press, New York, NY, United States
References: 19
Accession Number: 2021-036918
Categories: OceanographyGeochemistry of rocks, soils, and sediments
Document Type: Serial
Bibliographic Level: Analytic
Illustration Description: illus. incl. 4 tables, sketch map
N35°00'00" - N45°00'00", E130°00'00" - E140°00'00"
Country of Publication: United States
Secondary Affiliation: GeoRef, Copyright 2021, American Geosciences Institute. Reference includes data from GeoScienceWorld, Alexandria, VA, United States
Update Code: 2021
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