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Abstract
Blue opal from Peru is a new variety of gemstone. The comprehensive research on the gemmological features of this kind of blue opal shows that it is composed mainly of opal and minorly of α christobalite and α tridymite. At high temperature (1100℃), the opal, α christobalite and α tridymite in the blue opal are thermally transformed into β tridymite. The water in the blue opal occurs mainly in the form of planar water and structural water, with its Cu2+ impure ions tend to combine with H2O molecules into Cu2+(H2O)42+ hydrated ions. The presence of 761nm 2Eg→ 2T1g spin permitted transition absorption band in the octagonal crystal field indicates that the colouring of the blue opal is attributed mainly to Cu2+ (H2O)42+ hydrated ions.
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