Summary
Chalcophyllite is a rare secondary copper arsenate mineral occurring in the oxidized zones of some arsenic-bearing copper deposits. It was first described from material collected in Germany. At one time chalcophyllite from Wheal Tamar in Cornwall, England, was called tamarite, but this name is now discredited[2] (not to be confused with the amphibole mineral taramite, which is quite different). At Wheal Gorland a specimen exhibiting partial replacement of liriconite, Cu
2Al(AsO
4)(OH)
4·(4H
2O), by chalcophyllite has been found.[2] The mineral is named from the Greek, chalco "copper" and fyllon, "leaf", in allusion to its composition and platy structure. It is a classic Cornish mineral that can be confused with tabular spangolite.
| Chalcophyllite | |
|---|---|
 Chalcophyllite from the Ting Tang Mine, Carharrack, Cornwall, England. Photo by Rob Lavinsky | |
| General | |
| Category | Arsenate minerals |
| Formula (repeating unit) | Cu 18Al 2(AsO 4) 4(SO 4) 3(OH) 24·36(H 2O)[1][2][3] or Cu 18Al 2(AsO 4) 3(SO 4) 3(OH) 27·33(H 2O)[4][5][6] |
| IMA symbol | Chp[7] |
| Strunz classification | 8.DF.30 |
| Dana classification | 43.5.14.1 |
| Crystal system | Trigonal |
| Crystal class | Rhomboedral (3) H-M symbol: (3)[2][3][4][6] |
| Space group | R3[8] |
| Identification | |
| Color | Blue-green to emerald-green |
| Crystal habit | Crystals platy and six-sided, also as rosettes, drusy, foliated or massive. |
| Twinning | On {1010} as twin plane. |
| Cleavage | Perfect on {0001} |
| Fracture | Irregular |
| Mohs scale hardness | 2 |
| Luster | Vitreous to subadamantine, pearly on {0001} |
| Streak | Pale green |
| Diaphaneity | Transparent to translucent |
| Specific gravity | 2.67 to 2.69[3][4][6] or 2.4 to 2.66[5] |
| Optical properties | Uniaxial (−) |
| Refractive index | nω = 1.618 to 1.632, nε = 1.552 to 1.575 |
| Pleochroism | O blue-green, E almost colorless |
| Solubility | Soluble in acids and in ammonia |
| Other characteristics | Can be partially dehydrated. Alters to chrysocolla. Nonfluorescent, not radioactive |
| References | [8][3][4][5][6] |
Formula edit
Two different formulae are quoted in the literature for chalcophyllite, Cu
18Al
2(AsO
4)
4(SO
4)
3(OH)
24·36(H
2O)[1][2][3] (molar mass 3098 g) and Cu
18Al
2(AsO
4)
3(SO
4)
3(OH)
27·33(H
2O)[4][5][6] (molar mass 2956 g). The difference reflects the fact that the water content varies at room temperature based on relative humidity.[4]
Unit cell edit
Chalcophyllite crystallizes in the trigonal crystal class, 3 2/m with space group R 3m[5] or 3 with space group R 3.[2][3][4][6] Some authors choose a unit cell with three formula units per cell (Z = 3), and some a smaller unit cell with only 1.5 formula units per cell (Z = 1.5). For the larger unit cell a = 10.77 Å, c = 57.5 Å, Z = 3.[5][6][9] For the smaller unit cell c is only half as long, a = 10.756 Å, c = 28.678 Å, Z = 1.5.[3][4]
Crystal habit edit
Crystals are platy, six-sided and flattened perpendicular to the c crystal axis, and may be striated triangularly on these flattened faces. It may form rosettes, or be drusy, foliated or massive.[4]
Physical properties edit
Cleavage is perfect perpendicular to the c crystal axis, and twinning occurs with {1010} as the twin plane. Fracture is irregular. The mineral is soft, with hardness only 2, the same as gypsum. Specific gravity is generally given in the range 2.67 to 2.69, but Webmineral has 2.4 to 2.66. Chalcophyllite is soluble in acids and in ammonia. It is not fluorescent, nor radioactive. The water content varies at room temperature based on relative humidity. Chalcophyllite alters to chrysocolla,[4] which is a copper-aluminium silicate with the formula (Cu,Al)
2H
2Si
2O
5(OH)
4·n(H
2O).
Optical properties edit
Many copper minerals are blue or green in color; chalcophyllite is blue-green to emerald-green, with a pale green streak and vitreous to subadamantine luster, pearly on {0001}. Crystals are transparent to translucent. It is uniaxial (−) with refractive indices nω = 1.618 to 1.632 and nε = 1.552 to 1.575. Indices of refraction vary markedly depending on the relative humidity since the water content varies at ambient temperature.[4] It is pleochroic with O blue-green and E almost colorless.
Environment edit
Chalcophyllite is an uncommon secondary mineral occurring in the oxidized zones of some arsenic-bearing hydrothermal copper deposits. Associated minerals include azurite, malachite, brochantite, chrysocolla, spangolite, connellite, cuprite, cyanotrichite, strashimirite, parnauite, lavendulan, cornubite, langite, clinoclase, pharmacosiderite and mansfieldite.[3] The type material is conserved at the Mining Academy, Freiberg, Germany.[3] Notable occurrences include the Majuba Hill Mine, Antelope District, Nevada, US[2] and Cornwall, including Wheal Gorland, UK.
See also edit
References edit
- ^ a b "IMA Mineral List with Database of Mineral Properties".
- ^ a b c d e f g Rocks & Minerals (2009) 84-5: 434 to 440
- ^ a b c d e f g h i Handbook of Mineralogy
- ^ a b c d e f g h i j k Mindat.org
- ^ a b c d e f Webmineral data
- ^ a b c d e f g Gaines et al (1997) Dana's New Mineralogy, Wiley
- ^ Warr, L.N. (2021). "IMA–CNMNC approved mineral symbols". Mineralogical Magazine. 85 (3): 291–320. Bibcode:2021MinM...85..291W. doi:10.1180/mgm.2021.43. S2CID 235729616.
- ^ a b Mineralienatlas
- ^ Corbett (1973) American Mineralogist 58: 792–793
External links edit
- Crystal structure of chalcophyllite