Exact(41)
It forms a solid solution series with celestine, in which strontium replaces barium.
Ferrosilite, silicate mineral (Fe2Si2O6) and iron-rich end member of the orthopyroxene solid solution series.
Convergence regions of the solution series are determined.
Tetrahedrite forms a solid solution series with the similar mineral tennantite, in which arsenic replaces antimony in the molecular structure.
It forms a solid solution series with canfieldite in which tin replaces germanium in the crystal structure, which belongs to the isometric system.
Albite constitutes the sodium end-member of the plagioclase feldspar solid solution series and alkali feldspar series (see plagioclase; alkali feldspar).
Similar(19)
The plagioclase feldspars include members of the albite-anorthite solid-solution series.
Typically the name olivine is given to members of the forsterite-fayalite solid-solution series.
This mixture, called a solid-solution series, is a continuous chemical variation between the two pure substances.
It forms a complete solid-solution series with annabergite, in which nickel replaces cobalt in the erythrite structure.
In addition to the forsterite-fayalite series, other complete solid-solution series exist among the various olivine minerals.
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