The English name cinnabar jade is also known as "peony jade".

Originally discovered in Jilin in 1981, it was recently discovered at the top of a gold mine (commonly known as "Golden Red"). Its lithology is composed of quartz sand with cinnabar. The stone is hard and fine. Generally, the meat can not see its particles and is opaque. If the cinnabar is high, it can show the diamond luster, followed by the glass-grease luster. The color is red to pale red, the hardness is 7, and the relative density is 3-6 (depending on the content of cinnabar).

The bright red block containing the high cinnabar has a color ring like the silk agate (the color of the color ring is relatively dark), and a quartz fine vein cut through the color ring of about 0.1 mm is also common in the block. In addition to quartz and cinnabar, its constituent minerals contain barite, and there are granular anatase fillings in the pores and fissures.

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