Interstratified Clays as Fundamental Particles
作者： P. H. NADEAU , M. J. WILSON , W. J. MCHARDY , J. M. TAIT
DOI: 10.1126/SCIENCE.225.4665.923
关键词: Clay minerals 、 Materials science 、 Range (particle radiation) 、 Mineralogy 、 Chemical physics 、 Diffraction 、 Electron backscatter diffraction 、 Transmission electron microscopy 、 Elementary particle
摘要: Materials representing common interstratified clay minerals are shown to be composed of aggregates fundamental particles. Transmission electron microscopy and x-ray diffraction demonstrate that the characteristics a wide range interstratification can modeled experimentally by utilizing materials containing only three types The data have been incorporated into new model regards as populations particles whose patterns result from interparticle diffraction.
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M. J. Wilson, P. H. Nadeau, Interstratified Clay Minerals and Weathering Processes Springer, Dordrecht. pp. 97- 118 ,(1985) , 10.1007/978-94-009-5333-8_6
André Dunoyer de Segonzac, Roger Passeron, Henry Hugault, Dunoyer de Segonzac ,(1980)
Ed Perry, Burial Diagenesis in Gulf Coast Pelitic Sediments Clays and Clay Minerals. ,vol. 18, pp. 165- 177 ,(1970) , 10.1346/CCMN.1970.0180306
Per Aagaard, Harold C Helgeson, Activity/Composition Relations among Silicates and Aqueous Solutions: II. Chemical and Thermodynamic Consequences of Ideal Mixing of Atoms on Homological Sites in Montmorillonites, Illites, and Mixed-Layer Clays Clays and Clay Minerals. ,vol. 31, pp. 207- 217 ,(1983) , 10.1346/CCMN.1983.0310306
JOHN HOWER, ERIC V. ESLINGER, MARK E. HOWER, EDWARD A. PERRY, Mechanism of burial metamorphism of argillaceous sediment: 1. Mineralogical and chemical evidence Geological Society of America Bulletin. ,vol. 87, pp. 725- 737 ,(1976) , 10.1130/0016-7606(1976)87<725:MOBMOA>2.0.CO;2
P. H. Nadeau, M. J. Wilson, W. J. McHardy, J. M. Tait, The conversion of smectite to illite during diagenesis: evidence from some illitic clays from bentonites and sandstones Mineralogical Magazine. ,vol. 49, pp. 393- 400 ,(1985) , 10.1180/MINMAG.1985.049.352.10
Robert C. Reynolds, The Nature of Interlayering in Mixed-Layer Illite-Montmorillonites Clays and Clay Minerals. ,vol. 18, pp. 25- 36 ,(1970) , 10.1346/CCMN.1970.0180104
W. J. McHardy, M. J. Wilson, M. Tait, Electron microscope and X-ray diffraction studies of filamentous illitic clay from sandstones of the Magnus Field Clay Minerals. ,vol. 17, pp. 23- 40 ,(1982) , 10.1180/CLAYMIN.1982.017.1.04
P. H. Nadeau, J. M. Tait, W. J. McHardy, M. J. Wilson, Interstratified XRD Characteristics of Physical Mixtures of Elementary Clay Particles Clay Minerals. ,vol. 19, pp. 67- 76 ,(1984) , 10.1180/CLAYMIN.1984.019.1.07
G. DUNOYER SEGONZAC, THE TRANSFORMATION OF CLAY MINERALS DURING DIAGENESIS AND LOW-GRADE METAMORPHISM: A REVIEW Sedimentology. ,vol. 15, pp. 281- 346 ,(1970) , 10.1111/J.1365-3091.1970.TB02190.X