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砷硫锑铅矿(geocronite)原称斜方硫锑铅矿,其晶系经国外学者重新测定为单斜晶系而不属斜方晶系,主要化学成分常含一定量的砷,因而暂时改用现名。砷硫锑铅矿是一种较为罕见的硫盐矿物,国外报道的产地不多,每一产地在矿石中的含量也很稀少。我国迄今已知的砷硫锑铅矿产地有二:一为四川九龙斜卡,一为河北易县大南头。前者产状不明,但形成较大的块体出现;后者产于方铅矿-砷黝铜矿-石英-碳
Arsenic antimony antimony lead (geocronite) formerly known as orthomorphic antimony lead pyrite, the crystal system by the foreign scholars re-determined as monoclinic rather than orthorhombic system, the main chemical composition often contain a certain amount of arsenic, and therefore for the time being Change to the present name. Arsenic sulfur antimony lead ore is a relatively rare sulfur salt minerals, foreign origin reported in small quantities, each origin in the ore content is also very small. China has so far known arsenic antimony lead mine origin has two: one for Sichuan Kowloon ramp cards, one for the first line of Yixian County, Hebei Province. The former is unknown, but the formation of larger blocks appear; the latter is produced in galena - arsenic tetrahedrite - quartz - carbon