Endmember

An endmember in mineralogy is a mineral that is at the extreme end of a mineral series in terms of purity. Minerals often can be described as solid solutions with varying compositions of some chemical elements, rather than as substances with an exact chemical formula. There may be two or more endmembers in a group or series of minerals.

For example, the tectosilicate feldspar can be described as compositions of the endmembers K-feldspar [KAlSi₃O₈], albite [NaAlSi₃O₈] and anorthite [CaAl₂Si₂O₈].^[1] A specific feldspar can have varying quantities of potassium (K), sodium (Na) and calcium (Ca).

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