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The partial order domain is limited by the maximum order curve and the random order straight line (Fig. 13b). Segregation (R1) This type of stacking sequence is intermediate between random state and physical mixing (Fig. 13b). 35) Probabilities do not describe the heterogeneity of natural clay minerals in which at least two parameters may vary: the number of layers in a stacking sequence, and the proportion of each type of layer within this stacking sequence. Variations of the second parameter are described by Markovian probabilities applied to quasi-homogeneous structures (same number of layers in the stacking sequence for all crystals).

27 × 10−30 m3 . 68 × 104 g ·m−3 . The two other varieties of chlorite are: – donbassite, dioctahedral variety whose structure is derived from a pyrophyllite-like layer with the addition of a gibbsite-like octahedral sheet; – sudoite, di-trioctahedral variety, whose structure is derived from a pyrophyllite-like layer with the addition of a brucite-like octahedral sheet. Structure with Channelways: Palygorskite and Sepiolite The crystal structure of these two minerals differs from that of 1:1, 2:1 or 2:1:1 phyllosilicates.

No information can be obtained on those who have failed after formation. Analysis through frequency-size histograms of minerals may shed light on the progress of nucleation as a function of time. This has been performed on metamorphic rocks for which crystal counting is easier owing to their size. The data acquired certainly apply to clay rocks. 22 shows three types of distribution time 41 Nucleation and Crystal Growth: Principles corresponding to three different velocity ranges: increasing with time, constant or passing through a maximum (Kretz 1994).

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