| Reference Type | Journal (article/letter/editorial) |
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| Title | Thermomagnetic properties of banded manganiferous sediment from the Mid-Atlantic Ridge |
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| Journal | Canadian Journal of Earth Sciences |
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| Authors | Schwarz, E. J. | Author |
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| Year | 1968 (December 1) | Volume | 5 |
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| Issue | 6 |
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| Publisher | Canadian Science Publishing |
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| DOI | doi:10.1139/e68-149Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 472169 | Long-form Identifier | mindat:1:5:472169:1 |
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| GUID | 0 |
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| Full Reference | Schwarz, E. J. (1968) Thermomagnetic properties of banded manganiferous sediment from the Mid-Atlantic Ridge. Canadian Journal of Earth Sciences, 5 (6) 1517-1518 doi:10.1139/e68-149 |
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| Plain Text | Schwarz, E. J. (1968) Thermomagnetic properties of banded manganiferous sediment from the Mid-Atlantic Ridge. Canadian Journal of Earth Sciences, 5 (6) 1517-1518 doi:10.1139/e68-149 |
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| In | (1968, December) Canadian Journal of Earth Sciences Vol. 5 (6) Canadian Science Publishing |
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| Abstract/Notes | Banded manganiferous sediment from the Mid-Atlantic Ridge is paramagnetic at 20 °C and possibly has a Curie point at about −150 °C. Heating of the sediment in the range 520–560 °C prior to measuring probably results in the formation of a gradually changing ferrimagnetic spinel phase with a Curie point of 135 °C, which increases up to 180 °C. Heating to higher temperatures only results in a further increase in the relative abundance of the stable phase. |
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