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in the sulfur site. There is a complete series between canfieldite and its germanium analogue,
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Canfieldite was first described in 1893 from an occurrence in
Colquechaca,
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287:. The most typical form is as botryoidal rounded grape-like masses. Its
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is 6.28. Canfieldite exhibits conchoidal fracturing and no
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crystals which often appear to be cubic in form due to
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314:(1849–1926), an American mining engineer.
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350:"IMA–CNMNC approved mineral symbols"
329:List of minerals named after people
450:. You can help Knowledge (XXG) by
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271:substitution in the tin site and
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442:This article about a specific
1:
158:Irregular/ uneven, conchoidal
312:Frederick Alexander Canfield
148:Steel gray with reddish tint
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517:Minerals in space group 33
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16:Silver tin sulfide mineral
408:Mindat with location data
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259:mineral with formula: Ag
354:Mineralogical Magazine
522:Sulfide mineral stubs
512:Orthorhombic minerals
86:Strunz classification
375:10.1180/mgm.2021.43
366:2021MinM...85..291W
348:Warr, L.N. (2021).
310:. It was named for
233:6.2 – 6.3 g/cm
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279:. It forms black
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507:Sulfide minerals
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324:List of minerals
293:specific gravity
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112:Pyramidal (mm2)
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59:(repeating unit)
48:Sulfide minerals
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497:Silver minerals
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444:sulfide mineral
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419:Webmineral data
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397:Mineralienatlas
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291:is 2.5 and the
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360:(3): 291–320.
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140:Identification
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96:Crystal system
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289:Mohs hardness
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213:Greyish black
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108:Crystal class
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502:Tin minerals
452:expanding it
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306:Department,
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281:orthorhombic
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101:Orthorhombic
247:Canfieldite
219:Diaphaneity
126:Space group
33:Canfieldite
22:Canfieldite
491:Categories
335:References
277:argyrodite
249:is a rare
238:References
174:Mohs scale
117:H-M symbol
76:IMA symbol
384:235729616
273:tellurium
269:germanium
318:See also
297:cleavage
285:twinning
203:Metallic
177:hardness
164:Tenacity
154:Fracture
44:Category
362:Bibcode
308:Bolivia
257:sulfide
229:Density
189:⁄
168:Brittle
90:2.BA.70
55:Formula
39:General
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304:PotosĂ
251:silver
223:Opaque
209:Streak
199:Luster
115:(same
446:is a
380:S2CID
145:Color
448:stub
131:Pna2
370:doi
263:SnS
254:tin
80:Cfi
67:SnS
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358:85
356:.
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63:Ag
479:e
472:t
465:v
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265:6
261:8
191:2
187:1
184:+
182:2
134:1
119:)
69:6
65:8
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