湖南锡矿山锑矿床氧化带的自然硫  

NATIVE SULFUR IN THE OXIDIZED ZONE OF THE XIKUANGSHAN ANTIMONY ORE DEPOSIT,HUNAN

作　　者：蒋永年[1] 

机构地区：[1]地质矿产部天津地质矿产研究所,天津300170

出　　处：《矿物学报》1993年第3期263-267,共5页Acta Mineralogica Sinica

摘　　要：本文研究的自然硫产于锡矿山锑矿床氧化带底部。它的特点是晶体细小且晶面众多,其外貌颇似小的球状体。有关它的研究结果将为矿物学形态学以及晶体形态与成因的联系(成因形态学)提供新的资料,The native sulfur crystals examined in this paper occur at the bottomof the oxidized zone of the Xikuangshan Sb deposit and they are characterizedby fine size and extremely abundant crystal faces, rather resembling smallspherulites. This study will provide new clues to the crystal morphology as well as tothe relationship between crystal form and genesis (genetomorphology)

关 键 词：硫 锑 矿床 氧化带 晶体 形态学 

分 类 号：P618.660.4[天文地球—矿床学]