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USGS · 70010207

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

R. B. Finkelman
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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.

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R. B. Finkelman. 1970. Magnetic particles extracted from manganese nodules: Suggested origin from stony and iron meteorites. https://doi.org/10.1126/science.167.3920.982

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