Functions describing preferred orientation in flat aggregates of flake-like clay minerals and in other axially symmetric fabrics

Author:

Lippmann Friedrich

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Reference17 articles.

1. Braitsch, O.: Quantitative Auswertung einfacher Gefügediagramme. Heidelberger Beitr. Mineral. Petrog. 5, 210?226 (1956).

2. Brindley, G. W., and S. S. Kurtossy: Quantitative determination of kaolinite by X-ray diffraction. Am. Mineralogist 46, 1205?1215 (1961).

3. Dunn, C. G.: The analysis of quantitative pole-figure data. J. Appl. Phys. 25, 233?236 (1954).

4. Engelhardt, W. v., and K. H. Gaida: Concentration changes of pore solutions during the compaction of clay sediments. J. Sediment. Petrol. 33, 919?930 (1963).

5. Fisher, R. A.: Dispersion on a sphere. Proc. Roy. Soc. (London), Ser. A 217, 295?305 (1953).

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