Relation Between D.T.A. High Temperature Peak (850-1050 degrees C) of Montmorillonoid and Substitution of Cations in Lattice

Authors=KATO Chuzo

Journal/Book_names=Advances in Clay Science (3) - Proceedings of the Third Annual Meeting on Clays and Clay Minerals -

pages=13-20, 326-327

Publish_year=1961

Publish_Country=JPN

Publisher=Gihodo, Tokyo

Language_of_Text=JA

Language_of_Abs=EN

ID=196201012