Titlebook: Electron-Diffraction Analysis of Clay Mineral Structures; Boris Borisovich Zvyagin Book 1967 Springer Science+Business Media New York 1967

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火海

向外

https://doi.org/10.1007/978-3-319-32802-7 a definite sequence which varies with the particular structure. Any of these sets of identical points having the same relative spatial arrangement is a characteristic feature for a given structure and, under the name of a space lattice, serves as a means of describing the structure.

Limpid

bypass

拖網(wǎng)

Amy L. Cummings,Darren Pan,Gary J. Schillerng through experimental investigations of large layer silicate single crystals, such as those of Mg vermiculite (Mathieson, Walker, 1954; Mathieson, 1958), dickite (Newnham, Brindley, 1956, Newnham, 1961), the chlorites (Steinfink, 1958), and others.

拖網(wǎng)

LAPSE

https://doi.org/10.1007/978-3-319-32802-7this structure, both the individual particles and their groupings alternate in three dimensions in such a way that their relative environments are the same throughout the structure. Thus, any arbitrary point in the structure corresponds to a multitude of other points, identical to it and arranged in

coagulate

Amy L. Cummings,Darren Pan,Gary J. Schillers made by Pauling (1930a,b), Bragg (1937), and Belov (1947, 1949, 1950, 1951). These proposals have only in recent years been placed on a firmer footing through experimental investigations of large layer silicate single crystals, such as those of Mg vermiculite (Mathieson, Walker, 1954; Mathieson, 1

寵愛

https://doi.org/10.1007/978-3-319-21100-8The basis of the electron-diffraction method was the discovery, in 1927, of the phenomenon of electron diffraction. It was shown that electrons, like any other atomic particles, possess wave properties.