Magnetic particles extracted from manganese nodules: Suggested origin from stony and iron meteorites

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Abstract

On the basis of x-ray diffraction and electron microprobe data, spherical and ellipsoidal particles extracted from manganese nodules were divided into three groups. Group I particles are believed to be derived from iron meteorites, and Group II particles from stony meteorites. Group III particles are believed to be volcanic in origin.

Suggested Citation

Finkelman, R.B., 1970, Magnetic particles extracted from manganese nodules: Suggested origin from stony and iron meteorites: Science, v. 167, no. 3920, p. 982-984, https://doi.org/10.1126/science.167.3920.982.

Publication type Article
Publication Subtype Journal Article
Title Magnetic particles extracted from manganese nodules: Suggested origin from stony and iron meteorites
Series title Science
DOI 10.1126/science.167.3920.982
Volume 167
Issue 3920
Year Published 1970
Language English
Publisher American Association for the Advancement of Science
Description 3 p.
First page 982
Last page 984
Additional publication details