Geological Literature
Relation Between D.T.A. High Temperature Peak (850-1050 degrees C) of Montmorillonoid and Substitution of Cations in Lattice
KATO Chuzo
| item | description |
|---|---|
| Title | Relation Between D.T.A. High Temperature Peak (850-1050 degrees C) of Montmorillonoid and Substitution of Cations in Lattice |
| Authors | KATO Chuzo |
| Data name | Advances in Clay Science (3) - Proceedings of the Third Annual Meeting on Clays and Clay Minerals - |
| Page | 13-20, 326-327 |
| Year | 1961 |
| Publisher | Gihodo, Tokyo |
| Language | JA |
| Abstract language | EN |
| @id | https://gbank.gsj.jp/ld/resource/geolis/196201012 |