輝銻礦
Sb2S3
Stibnite is a sulfide mineral known for its striking metallic crystals, with several world-class Chinese localities.
Stibnite — the principal ore of antimony — is one of the most distinctive sulfides in collecting. Its long silvery blades, radiating into starburst sprays, are a signature look of Chinese mineralogy. A published geological study describes the Xikuangshan deposit in Hunan as the world’s largest antimony deposit; it is also documented for bladed stibnite specimens.
The Chinese angle
The Xikuangshan and Wuning deposits yield individual stibnite crystals in excess of 30 cm — including the legendary Houluoping pocket whose blades resembled polished steel sabers. Chinese stibnite is the worldwide reference for the species; nothing else comes close in size or perfection.
Localities and the great pockets
Xikuangshan (Lengshuijiang) in central Hunan is the world’s largest antimony deposit and the reference source for the species — bladed and prismatic crystals with a bright metallic lustre, sometimes in radiating sprays, on crystalline calcite or with barite. The Wuning area of Jiangxi adds further fine material.
Judging quality, value, and care
Length, blade sharpness, metallic lustre, and freedom from cleavage damage — to which this soft, perfectly-cleaved sulfide is prone — all drive value; undamaged terminations and minimal tarnish are key. Stibnite tarnishes slowly in humid air, so store it with a desiccant in low light, keep it away from sulfur-laden materials, and never clean it with acids. See the Lengshuijiang page.
現有標本

Gray Stibnite — Bulgaria

Gray Stibnite with Calcite — Lengshuijiang, Hunan, China

Gray Stibnite with Quartz — Lengshuijiang, Hunan, China

輝銻礦晶體伴母岩,中國湖南

輝銻礦晶簇 – 中國湖南 – 7.6 × 5.1 cm

輝銻礦晶簇伴重晶石 – 湖南冷水江

放射狀輝銻礦刃狀晶體伴方解石 – 中國湖南
