"' Cesanite "'is the end member of the apatite-wilkeite-ellestadite series that substitutes all of apatite's phosphate ions with sulfate ions and balances the difference in charge by replacing several calcium ions with sodium ions.
32.
Beyond that, there appear to be five types of bone-growth, which may represent five natural groupings within the thelodonts or a spectrum ranging between the end members meta-( or ortho-) dentine and mesodentine tissues.
33.
Given a chance to face Braves fifth starter Terrell Wade and four low-end members of the bullpen, the Dodgers rapped out 13 hits _ their second-highest total this season _ with many sharing in the fortune.
34.
End member formation ( jarosite and natrojarosite ) is favoured by a low temperature environment, less than 100 �C, and is illustrated by the oscillatory zoning of jarosite and natrojarosite found in samples from the Apex Mine, Arizona, and Gold Hill, Utah.
35.
In the jarosite-natrojarosite series Na substitutes for K to at least Na / K = 1 : 2.4 but the pure sodium end member NaFe 3 + 3 ( SO 4 ) 2 ( OH ) 6 is not known in nature.
36.
The end members of the group were named hydroxylellestadite ( X = OH ), fluorellestadite ( X = F ) and chlorellestadite ( X = Cl ); ideal end-member chlorellestadite is assumed not to exist in nature, although it has been synthesized.
37.
An extensive solid solution exists between the two end members wulfenite and stolzite ( PbWO 4 ), such that tungstenian-wulfenite compositions range from 90 % wulfenite and 10 % stolzite to chillagite ( 64 % wulfenite, 36 % stolzite ) and so on.
38.
A valid end member interpretation is that the crater population still represents a population emplaced on a mostly inactive planet, but the final throes of a global emplacement of volcanic plains has filled most of the craters with a few hundred meters of volcanic flows.
39.
There is a spectrum of turbidity-or density-current types ranging from " muddy water " to massive mudflow, and evidence of both these end members can be observed in deposits associated with the deeper parts of submarine canyons and channels, such as lobate deposits ( mudflow ) and levees along channels.
40.
For example, the plagioclase feldspars comprise a continuous series from sodium-rich end member albite ( NaAlSi 3 O 8 ) to calcium-rich anorthite ( CaAl 2 Si 2 O 8 ) with four recognized intermediate varieties between them ( given in order from sodium-to calcium-rich ) : oligoclase, andesine, labradorite, and bytownite.
