Abstract
Fe substitution for A1 in kaolinite (from Venezuelan laterites) is proved by infrared spectroscopy and chemical techniques.-from Authors English
| Original language | English |
|---|---|
| Pages (from-to) | 323-331 |
| Number of pages | 9 |
| Journal | Clay Minerals |
| Volume | 14 |
| Issue number | 4 |
| DOIs | |
| State | Published - 1979 |
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