The yellow seal stone from northern Laos is one possible substitute for the Tianhuang Stone, the most famous Chinese seal stone, because of its similar yellow to orange-yellow appearance and the same main mineral composition. The colour causation of the yellow seal stone from northern Laos was studied. The samples’ phase, micro-morphology and chemical components were studied by Raman spectroscopy, and scanning electron microscopy (SEM) with energy disperse spectroscopy (EDS), respectively. The yellow seal stone from northern Laos is mainly composed of dickite, occasionally with minor impurity minerals, such as hematite, anatase, barite, diaspore and pyrite. Micro- to nano-sized iron oxides/hydroxides were observed and detected by SEM and EDS in the yellow to orange-yellow part of the samples. Moreover, these iron oxides/hydroxides were suggested to cause the yellow to orange-yellow in the seal stone from northern Laos. The UV-Vis spectrum and its second derivative, the Kubelka-Munk spectra, were used to identify and quantify hematite and goethite. The samples’ colour parameters were obtained with the Commission Internationale de l’Eclairage (CIE) 1931 standard space. According to the observation of the samples and the results obtained from experiments and calculations, the colour of the yellow parts (L* = 33.56~47.99, a* = 0.35~3.65, b* = 4.55~9.89) correlated with goethite (goethite is about 0.175~0.671 g/kg, the content of hematite was too low to be figured out in the yellow parts). In contrast, the colour of the orange-yellow parts (L* = 33.99~46.27, a* = 3.98~12.39, b* = 8.04~22.14) was more closely related with the content of hematite (goethite is about 0.096~0.691 g/kg, hematite is about 0.258~2.383 g/kg). The results of correlation analysis also support that the contents of iron oxides or hydroxides influence the samples’ colour. Therefore, it is suggested that micro- to nano-scaled hematite and goethite caused the colour of yellow and orange-yellow in the studied seal stone. Hematite can strengthen the red hue and change the colour from yellow to orange-yellow.

Hessonite, a special variety of grossularite, is well-known for the heat-wave effect, which is a characteristic swirled or roiled interior appearance within the crystal. Although the heat-wave effect has been observed for a long time, it has not been studied in depth. In this study, the gemological properties, mineral compositions, fabric characteristics, and grain sizes of hessonite samples were investigated using infrared spectroscopy, electron backscatter diffraction (EBSD), and energy-dispersive X-ray spectroscopy (EDS). Hessonite exhibits the heat-wave effect and is found to be polycrystal rather than single-crystal, composed of submillimeter-sized granules with random orientation and limited variations in Fe and Al contents. Abundant micropores exist among the granules, indicating imperfect contact among them. Due to these structural features, incident light is interrupted and undergoes changes in direction and speed as it passes through the hessonite granules, grain borders, and micropores. Light reflects off the granules’ surfaces and refracts within the granules, respectively, causing the incident light to swirl and roil within the hessonite and form the heat-wave effect. This study considers that the heat-wave effect is a special optical phenomenon not caused by impurity minerals or inclusions.