| 词条 | Kobellite |
| 释义 |
| name = Kobellite | boxwidth = | boxbgcolor = | image = Kobellite-540285.jpg | imagesize = | alt = | caption = | category = Sulfide minerals | formula = Pb22Cu4(Bi,Sb)30S69 | molweight = | strunz = 2.HB.10a | system = Orthorhombic | class = Dipyramidal (mmm) H-M symbol: (2/m 2/m 2/m) | symmetry = P21/n | unit cell = | color = | colour = | habit = | twinning = | cleavage = | fracture = | tenacity = | mohs = | luster = | streak = | diaphaneity = | gravity = | density = | polish = | opticalprop = | refractive = | birefringence = | pleochroism = | 2V = | dispersion = | extinction = | length fast/slow = | fluorescence = | absorption = | melt = | fusibility = | diagnostic = | solubility = | impurities = | alteration = | other = | prop1 = | prop1text = | references = [1][2][3] }} Kobellite (Pb22Cu4(Bi,Sb)30S69) is a gray, fibrous, metallic mineral. It is also a sulfide mineral consisting of antimony, bismuth, and lead. It is a member of the izoklakeite - berryite series with silver and iron substituting in the copper site and a varying ratio of bismuth, antimony, and lead. It crystallizes with monoclinic pyramidal crystals. The mineral can be found in ores and deposits of Hvena, Sweden; Ouray, Colorado; and Wake County, North Carolina, US. The mineral was named after Wolfgang Franz von Kobell (1803–1882), a German mineralogist. See also
References1. ^[https://www.mineralienatlas.de/lexikon/index.php/MineralData?mineral=Kobellite] {{sulfide-mineral-stub}}2. ^Mindat.org 3. ^Webmineral.com 6 : Lead minerals|Copper minerals|Bismuth minerals|Antimony minerals|Sulfosalt minerals|Orthorhombic minerals |
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