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Relation Between D.T.A. High Temperature Peak (850-1050 degrees C) of Montmorillonoid and Substitution of Cations in Lattice
KATO Chuzo
itemdescription
TitleRelation Between D.T.A. High Temperature Peak (850-1050 degrees C) of Montmorillonoid and Substitution of Cations in Lattice
AuthorsKATO Chuzo
Data nameAdvances in Clay Science (3) - Proceedings of the Third Annual Meeting on Clays and Clay Minerals -
Page13-20, 326-327
Year1961
PublisherGihodo, Tokyo
LanguageJA
Abstract languageEN
GEOLIS URLhttps://darc.gsj.jp/archives/detail?cls=geolis&pkey=196201012
@idhttps://gbank.gsj.jp/ld/resource/geolis/196201012