| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 1695672 | Applied Clay Science | 2010 | 6 Pages |
Abstract
⺠PAS and EPR studies showed the presence of Mn2+ and Fe3+ ions in serpentines. ⺠Mn2+ occupied octahedral Mg2+ sites. ⺠Fe3+ occupied mainly tetrahedral Si sites and a few octahedral Mg2+ sites. ⺠A broad EPR signal observed in some samples were attributed to presence of Fe clusters or MgFe2O4.
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Related Topics
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Earth and Planetary Sciences
Geochemistry and Petrology
Authors
Arijit Sengupta, R.M. Kadam, B. Rajeswari, A.R. Dhobale, Y. Babu, S.V. Godbole,