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 |
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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 |
GEOLIS URL | https://darc.gsj.jp/archives/detail?cls=geolis&pkey=196201012 |
@id | https://gbank.gsj.jp/ld/resource/geolis/196201012 |