Diagenesis of Dioctahedral and Trioctahedral Smectites From Alternating Beds in Miocene to Pleistocene Rocks of the Niigata Basin, Japan
Clays and Clay Minerals - United States
doi 10.1346/ccmn.2001.0490407
Full Text
Open PDFAbstract
Available in full text
Date
January 1, 2001
Authors
Publisher
Springer Science and Business Media LLC