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・ Kermanshah Province
・ Kermanshah University of Medical Sciences
・ Kermanshahis
・ Kermaran
・ Kermaria-Sulard
・ Kermath
・ Kermejegan
・ Kermen
・ Kermen Peninsula
・ Kermes
・ Kermes (dye)
・ Kermes (insect)
・ Kermes mineral
・ Kermes vermilio
・ Kermesidae
Kermesite
・ Kermess
・ Kermesse
・ Kermesse (cycling)
・ Kermesse (festival)
・ Kermestan
・ Kermet Apio
・ Kermeta
・ Kermeter
・ Kermeur Sandstone
・ Kermi
・ Kermia
・ Kermia aegyptiaca
・ Kermia aglaia
・ Kermia albicaudata


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Kermesite : ウィキペディア英語版
Kermesite

Kermesite or antimony oxysulfide is also known as red antimony (Sb2S2O) . The mineral’s color ranges from cherry red to a dark red to a black. Kermesite is the result of partial oxidation between stibnite (Sb2S3) and other antimony oxides such as valentinite (Sb2O3) or stibiconite (Sb3O6(OH)). Under certain conditions with oxygenated fluids the transformation of all sulfur to oxygen would occur but kermesite occurs when that transformation is halted.

==Mining and specimens==
Deposits of this mineral have been found all over the world, however notable deposits have been found in Braunsdorf, near Freiberg, Saxony, Germany; Pernek, Pezinok, and Pribram, Czechoslovakia; the Lac Nicolet mine, South Ham Township, Wolfe County, Quebec, Canada; Sombrerete, Zacatecas, Mexico; Santa Cruz and San Francisco mines, Poopo, Oruro, Bolivia; Que Que, Zimbabwe; Djebel Haminate, Algeria; Broken Hill, New South Wales, Australia; Mohave, Kern County, California and Burke, Shoshone County, Idaho.〔〔Palache, C., H. Berman, and C. Frondel (1944) ''Dana's System of Mineralogy,'' Wiley, 7th ed., v. I, pp. 279-280〕

抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)
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