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Pyroclastic density currents (PDCs) vary between two end members, concentrated and dilute.
Furthermore, the heat carrying phonons are strongly scattered with increasing x value because of the formation of solid solutions between two end members: □FeSb2Te and □FeSb3 (where □ can be viewed as a vacancy).
Specifically, all deep water below the CIL falls on roughly a linear relationship between two end members, the CIL and the Lower Bosporus inflow.
These studies demonstrated that the concentration of solutes of mixtures between two end members follows a linear relation, while chemical reactions of reactive constituents introduce significant non-linear effects (Wigley and Plummer 1976).
Several studies suggested boundary zones intermediate between two end members.
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Microbialites are typically transitional between four end members: (1) cuspate microbialites, (2) plumose microbialites, (3) stratiform, domal and columnar microbialites, and (4) incipient microbialites.
Assimilation of foreign material into a granitic magma body entails mixing between two end-member components: the initially solid assimilant, and the original magma, whose composition is mostly represented by a granitic liquid.
We suggest that the commonly observed case of age decreasing with grain size in K Ar and 40Ar/39Ar dating of brittle fault rocks can be interpreted as a consequence of mixing between two end-member illite/muscovite generations: an authigenic and a protolithic, in which the finest authigenic grains constrain the timing of the last faulting increment.
Rather, they tended to oscillate between two end-member quasi-steady-state profiles.
The interaction between the two end members was analyzed both chemically and mechanically.
The step speed reduction effect can be explained in light of the slower growth kinetics of otavite with respect to pure calcite and the fact that the first layer grown has an intermediate composition between the two end members.
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