List of minerals (synonyms)

Last updated

The International Mineralogical Association (IMA) is the international group that recognises new minerals and new mineral names. However, minerals discovered before 1959 did not go through the official naming procedure although some minerals published previously have been either confirmed or discredited since that date.

Contents

List of main synonyms

Mainly renamed minerals and synonyms used by the Handbook of Mineralogy. [1]

A

B

C

D–E

F–G

H–J

K–L

M

N-O

P–R

S

T

U–Z

Mineral varieties

Mainly minerals varieties used by the Handbook of Mineralogy.

  1. Iridosmine*, an osmium variety, 01.AF.05
  2. Plagioclase solid solution series:
    1. An0: albite; An20: oligoclase; An40: andesine; An60: labradorite; An80: bytownite; An100: anorthite
    2. Oligoclase, albite variety, 09.FA.35
    3. Andesine, albite variety, 09.FA.35
    4. Labradorite, anorthite variety, 09.FA.35
    5. Bytownite, anorthite variety, 09.FA.35
  3. Ilmenorutile, a rutile variety, 04.DB.05
  4. Incaite*, a franckeite variety, 02.HF.25b
  5. Kamacite, a native iron variety, 01.AE.05
  6. Kerolite* (discredited 1979), a Ni-bearing variety of talc (?), 09.EC.05, [no]
  7. Lewistonite* (discredited 1978), a carbonate-rich variety of fluorapatite, 08.BN.05 [no]
  8. Metaberyllite* (Y: 1973, discredited 2006), a variety of beryllite, 09.AE.05, [no]
  9. Potosiite*, a franckeite variety, 02.HF.25b
  10. Sakharovaite* (Y: 1956, discredited 2006), a Bi-bearing variety of jamesonite, 02.HB.15,
  11. Struverite*, a rutile variety, 04.DB.05

Doubtful procedures

Unnamed minerals, controversial discreditations

  • Scandian ixiolite (of von Knorring)N, a Nb-bearing variety of ixiolite, 04.DB.25; possibly a separate species. [5] [6]
  • Scandian ixiolite (of Bergstol)N, a Sc-bearing variety of ixiolite, 04.DB.25; possibly a separate species. [7] [8]
  • Ktenasite (Y: 1950) 07.DD.20, possibly a mineral group, under review (Leverett et al., 2009–2011). [9]
  • Unnamed (Zn-analogue of Ktenasite)N. [10]
  • Unnamed (Co-analogue of Ktenasite)N. [11]
  • Mg- or Cd-bearing varieties are also known.
  • Mitchell R H, Burns P C, Chakhmouradian A R (2000) The crystal structures of loparite-(Ce), The Canadian Mineralogist 38, 145-152.
  • Zubkova, N. V., Arakcheeva, A. V., Pushcharovskii, D. Y., Semenov, E. I., & Atencio, D. (2000). Crystal structure of loparite. Crystallography Reports, 45(2), 210-214.
  • Calciogadolinite-Y? (Y: 1938) might be a calcian gadolinite. [13] [14]
  • Clinotyrolite N (monoclinic), both minerals might belong to a mineral group since tyrolite was shown to be monoclinic (pseudo-orthorhombic). [15]
  • Yttromicrolite-(Y) within the framework of nomenclature of Hogarth (1977): discreditation was not made by proper way (in the course of defamation of Crook, 1982). [16]
  • Pimelite* (Y: 1800, 1938) a nickel dominant smectite, is under review. Associations: nickel-bearing talc, yellow green nickeloan nontronite, red brown hematite stained nontronite, bright white montmorillonite. [17] [18] [19]
  • Tetranatrolite (discredited in 1999): might be identical to gonnardite, discreditation procedure apparently done without actually working on the type specimen or on any identified tetranatrolite itself. [20] [21] [22]
  • Yftisite-(Y) (discredited in 1987): but apparently the cell parameters are known (Balko & Bakakin, 1975). [23]
  • Buserite (IMA1970-024): dehydrates to birnessite, known synthetic compound. [24] [25] [26]
  • Zincobotryogen: it is discredited (IMA1967 s.p.) but its crystal structure has been solved (space group 14). [27]
  • Strontioborite: it is discredited (IMA1962 s.p.) but its crystal structure has been solved (space group 4). [28]
  • Aguilarite (Y: 1944, Ag4SeS, 2.BA.55): it might be two solid solution series, a monoclinic 'acanthite-like' series (from Ag2S - Ag2S0.4Se0.6), and an orthorhombic 'naumannite-like' series (from Ag2S0.3Se0.7 - Ag2Se). [29]

Controversial chemical formulas (IMA Master List)

(and/or possible "analytical" artifacts)
  • Kobeite-Y (Y: 1950) 04.DG.05, the original analytical determinations contain between 14.91% and 17.08% ZrO2 with only 1.99% and 1.59% SiO2 respectively. The chemical formula (IMA version: (Y,U)(Ti,Nb)2(O,OH)6) doesn't contain Zr.
  • Divalent sulfide. Mackinawite (Y: 1963) 02.CC.25 (IMA formula: (Fe,Ni)
    1+x
    S
    ()), sulfide anion (atoms per formula unit, apfu) might be too low due to analytical losses. [34] [35] [36]
  • Pseudo monovalent mercury, mindat.org changed the chemical formulas: there is mercury(II) and (dimercury) [Hg-Hg] now.
Notes:
  • Claraite (IMA2016-L, IMA1981-023) 05.DA.30 (IMA formula: Cu2+3CO3(OH)4·4H2O), but after U. Kolitsch it has essential As and S. [37]
  • Kolitsch, U. & Brandstätter, F. (2012): 1743) Baryt, Chalkophyllit und Clarait vom Pengelstein bei Kitzbühel, Tirol. P. 149. in Niedermayr, G. et al. (2012): Neue Mineralfunde aus Österreich LX. Carinthia II, 202./122., 123-180.
  • Putz, H., Lechner, A. & Poeverlein, R. (2012): Erythrin und Clarait vom Pichlerstollen am Silberberg bei Rattenberg, Nordtirol. Lapis, 37 (1), 47-52; 62.
  • New chemical formula: (Cu,Zn)15(CO3)4(AsO4)2(SO4)(OH)14·7H2O.
  • Cosalite (Y: 1868) 02.JB.10 (IMA formula: Pb2Bi2S5). It might have copper as essential constituent (AM Clark, MH Hey (1993) Hey's mineral index: mineral species, varieties and synonyms), (Zak, L.; Megarskaya, L.; Mumme, W. G. (1992). "Rezbanyite from Ocna de fier (Vasko): a mixture of bismuthinite derivatives and cosalite". Neues Jahrbuch für Mineralogie. Monatshefte 1992: 69–79.).
  • The general structural formula for cosalite can be expressed as: CuxAg(i + s)Pb[8–2s–0.5(x + i)]Bi(8 + s)S20. [38]
  • Mayenite (IMA2013-C, IMA1963-016): it can not be found in nature. Mayenite (stabilized by moisture) can be found in cement industry chemistry. Chlormayenite can be found in nature.

Suspended (IMA status)

  • (IMA2000-026) (Mn,Li)4(Ta,Sn)4(Ta,Nb)8O32: IMA approval status is suspended, but it was incorrectly stated as approved in Grice, J.D. & Ferraris, G. (2001). [39]
  • (IMA1989-012), zhangpeishanite (of Shen), unnamed (cordylite-like (Ca□Ba2Ce4[CO3]8F2). [40]

Grandfathered (IMA valid species)

Rejected or discredited minerals

Errors and synonyms

Non minerals

Discredited mineral varieties

Discredited polytypes

See polytype section

Groups and pairs

Amphibole dump

Discredited, renamed and/or hypothetical amphiboles

Polytypes

Based on Nickel (1993). [48]

Synonyms, discredited polytypes

Under construction

Hydrous diuranyl di(RO4) family

Meta-autunite group

Natroautunite group

Carnotite family (partial)

Other hydrous families

Hydrotalcite supergroup

The hydrotalcite supergroup might need another review. [55]

Hydrotalcite group
Suggested: Mg
6
Mn3+
2
(OH)
16
[CO
3
]·4H
2
O
Suggested: Ni
6
Fe3+
2
(OH)
16
Cl
2
·4H
2
O
Suggested: Mg6Al2(OH)16[CO3]·4H2O
  • Iowaite A (1967-002), chemical formula
Suggested: Mg
6
Fe3+
2
(OH)
16
Cl
2
·4H
2
O
Suggested: possibly Ni2+
6
Ni3+
2
(OH)
16
S·4H
2
O
Suggested: Mg
6
Al
2
(OH)
16
(OH)
2
·4H
2
O
Suggested: Mg
6
Fe3+
2
(OH)
16
[CO
3
]·4H
2
O
Suggested: Ni
6
Fe3+
2
(OH)
16
[CO
3
]·4H
2
O
Suggested: Mg6Cr2(OH)16[CO3]*4H2O
  • Takovite A (Y: 1957, 1977 s.p.), chemical formula
Suggested: Ni6Al2(OH)16[CO3]·4H2O
Suggested: Mg6Cr2(OH)16Cl2·4H2O
Quintinite group
  • Caresite A (1992-030), chemical formula
Suggested: Fe3+
4
Al
2
(OH)
12
[CO
3
]·3H
2
O
Suggested: Mn4Al2(OH)12[CO3]·3H2O
Suggested: Mg4Al2(OH)12Cl2·2H2O
Suggested: Ni
4
Co3+
2
(OH)
12
[CO
3
]·3H
2
O
Suggested: Mg4Al2(OH)12[CO3]·3H2O
Suggested: Zn4Al2(OH)12[CO3]·3H2O
Fougèrite group
Suggested: Fe2+
4
Fe3+
2
(OH)
12
[CO
3
]·3H
2
O
Suggested: Fe3+
6
O
4
(OH)
8
[CO
3
]·3H
2
O
Suggested: Fe2+
2
Fe3+
4
O
2
(OH)
10
[CO
3
]·3H
2
O
Woodwardite group
Suggested:
Suggested:
Suggested:
Cualstibite group
Suggested: Cu2Al(OH)6[Sb(OH)6]
  • Omsite A (2012-025), chemical formula
Suggested: Ni
2
Fe3+
(OH)
6
[Sb(OH)
6
]
Suggested: Zn2Al(OH)6[Sb(OH)6]
Glaucocerinite group
Suggested:
Suggested:
Suggested:
Suggested:
Suggested:
Suggested:
Wermlandite group
Suggested: Mg18Al9(OH)54Sr2(CO3)9(H2O)6(H3O)5
Suggested: Mg6Al3(OH)18[Na(H2O)6](SO4)2·6H2O, possibly more than one species
Suggested: possibly Zn6Al3(OH)18[Na(H2O)6](SO4)2·6H2O
Suggested: Fe2+
6
Al
3
(OH)
18
[Na(H
2
O)
6
](SO
4
)
2
·6H
2
O
  • Shigaite A (1984-057), chemical formula
Suggested: Mn6Al3(OH)18[Na(H2O)6](SO4)2·6H2O
Suggested: Mg7Al2(OH)18[Ca(H2O)6](SO4)2·6H2O
Hydrocalumite group
Suggested: Ca4Al2(OH)12(Cl,CO3,OH)2·4H2O, possibly multiple species
  • Kuzelite A (1996-053), chemical formula
Suggested: Ca4Al2(OH)12(SO4)·6H2O

See also

Further reading

Related Research Articles

<span class="mw-page-title-main">Silicate mineral</span> Rock-forming minerals with predominantly silicate anions

Silicate minerals are rock-forming minerals made up of silicate groups. They are the largest and most important class of minerals and make up approximately 90 percent of Earth's crust.

<span class="mw-page-title-main">Kalinite</span>

Kalinite is a mineral composed of hydrated potassium aluminium sulfate. It is a fibrous monoclinic alum, distinct from isometric potassium alum, named in 1868. Its name comes from kalium (derived from Arabic: القَلْيَه al-qalyah "plant ashes", which is the Latin name for potassium, hence its chemical symbol, "K".

<span class="mw-page-title-main">Vauxite</span> Phosphate mineral

Vauxite is a phosphate mineral with the chemical formula Fe2+Al2(PO4)2(OH)2·6(H2O). It belongs to the laueite – paravauxite group, paravauxite subgroup, although Mindat puts it as a member of the vantasselite Al4(PO4)3(OH)3·9H2O group. There is no similarity in structure between vauxite and paravauxite Fe2+Al2(PO4)2(OH)2·8H2O or metavauxite Fe3+Al2(PO4)2(OH)2·8H2O, even though they are closely similar chemically and all minerals occur together as secondary minerals. Vauxite was named in 1922 for George Vaux Junior (1863–1927), an American attorney and mineral collector.

<span class="mw-page-title-main">Chloritoid</span>

Chloritoid is a silicate mineral of metamorphic origin. It is an iron magnesium manganese alumino-silicate hydroxide with formula (Fe, Mg, Mn)
2
Al
4
Si
2
O
10
(OH)
4
. It occurs as greenish grey to black platy micaceous crystals and foliated masses. Its Mohs hardness is 6.5, unusually high for a platy mineral, and it has a specific gravity of 3.52 to 3.57. It typically occurs in phyllites, schists and marbles.

<span class="mw-page-title-main">Ferrihydrite</span> Iron oxyhydroxide mineral

Ferrihydrite (Fh) is a widespread hydrous ferric oxyhydroxide mineral at the Earth's surface, and a likely constituent in extraterrestrial materials. It forms in several types of environments, from freshwater to marine systems, aquifers to hydrothermal hot springs and scales, soils, and areas affected by mining. It can be precipitated directly from oxygenated iron-rich aqueous solutions, or by bacteria either as a result of a metabolic activity or passive sorption of dissolved iron followed by nucleation reactions. Ferrihydrite also occurs in the core of the ferritin protein from many living organisms, for the purpose of intra-cellular iron storage.

<span class="mw-page-title-main">Layered double hydroxides</span> Class of ionic solids characterized by a layered structure

Layered double hydroxides (LDH) are a class of ionic solids characterized by a layered structure with the generic layer sequence [AcB Z AcB]n, where c represents layers of metal cations, A and B are layers of hydroxide anions, and Z are layers of other anions and neutral molecules. Lateral offsets between the layers may result in longer repeating periods.

<span class="mw-page-title-main">Tschermakite</span> Amphibole, double chain inosilicate mineral

The endmember hornblende tschermakite (☐Ca2(Mg3Al2)(Si6Al2)O22(OH)2) is a calcium rich monoclinic amphibole mineral. It is frequently synthesized along with its ternary solid solution series members tremolite and cummingtonite so that the thermodynamic properties of its assemblage can be applied to solving other solid solution series from a variety of amphibole minerals.

<span class="mw-page-title-main">Arthurite</span>

Arthurite is a mineral composed of divalent copper and iron ions in combination with trivalent arsenate, phosphate and sulfate ions with hydrogen and oxygen. Initially discovered by Sir Arthur Russell in 1954 at Hingston Down Consols mine in Calstock, Cornwall, England, arthurite is formed as a resultant mineral in the oxidation region of some copper deposits by the variation of enargite or arsenopyrite. The chemical formula of Arthurite is CuFe23+(AsO4,PO4,SO4)2(O,OH)2·4H2O.

<span class="mw-page-title-main">Chalcophyllite</span>

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. At Wheal Gorland a specimen exhibiting partial replacement of liriconite, Cu
2
Al(AsO
4
)(OH)
4
·(4H
2
O)
, by chalcophyllite has been found. 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.

<span class="mw-page-title-main">Cabalzarite</span>

Cabalzarite is a rare arsenate mineral with the chemical formula Ca(Mg,Al,Fe3+
)
2
[AsO
4
]
2
•2(H
2
O,OH)
. It is a member of the tsumcorite group. It crystallizes in the monoclinic system and typically occurs as clusters of crystals or granular aggregates.

<span class="mw-page-title-main">Tsumebite</span>

Tsumebite is a rare phosphate mineral named in 1912 after the locality where it was first found, the Tsumeb mine in Namibia, well known to mineral collectors for the wide range of minerals found there. Tsumebite is a compound phosphate and sulfate of lead and copper, with hydroxyl, formula Pb2Cu(PO4)(SO4)(OH). There is a similar mineral called arsentsumebite, where the phosphate group PO4 is replaced by the arsenate group AsO4, giving the formula Pb2Cu(AsO4)(SO4)(OH). Both minerals are members of the brackebuschite group.

Nabalamprophyllite has a general formula of Ba(Na,Ba){Na3Ti[Ti2O2Si4O14](OH,F)2}. The name is given for its composition and relation to other lamprophyllite-group minerals. Lamprophyllite is a rare Ti-bearing silicate mineral usually found in intrusive igneous rocks.

<span class="mw-page-title-main">Chesterite</span>

Chesterite is a rare silicate mineral that can be compared to amphiboles, micas, and jimthompsonite. Its chemical formula is (Mg,Fe)
17
Si
20
O
54
(OH)
6
. Chesterite is named after Chester, Vermont, where it was first described in 1977. The specific geologic setting within its origin is the Carleton talc quarry in Chester, Vermont.

<span class="mw-page-title-main">Pearceite</span>

Pearceite is one of the four so-called "ruby silvers", pearceite Cu(Ag,Cu)6Ag9As2S11, pyrargyrite Ag3SbS3, proustite Ag3AsS3 and miargyrite AgSbS2. It was discovered in 1896 and named after Dr Richard Pearce (1837–1927), a Cornish–American chemist and metallurgist from Denver, Colorado.

<span class="mw-page-title-main">Ferrogedrite</span> Amphibole, double chain inosilicate mineral

Ferrogedrite is an amphibole mineral with the complex chemical formula of ☐Fe2+2(Fe2+3Al2)(Si6Al2)O22(OH)2. It is sodium and calcium poor, making it part of the magnesium-iron-manganese-lithium amphibole subgroup. Defined as less than 1.00 apfu (atoms per formula unit) of Na + Ca and consisting of greater than 1.00 apfu of (Mg, Fe2+, Mn2+, Li) separating it from the calcic-sodic amphiboles. It is related to anthophyllite amphibole and gedrite through coupled substitution of (Al, Fe3+) for (Mg, Fe2+, Mn) and Al for Si. and determined by the content of silicon in the standard cell.

<span class="mw-page-title-main">Köttigite</span>

Köttigite is a rare hydrated zinc arsenate which was discovered in 1849 and named by James Dwight Dana in 1850 in honour of Otto Friedrich Köttig (1824–1892), a German chemist from Schneeberg, Saxony, who made the first chemical analysis of the mineral. It has the formula Zn3(AsO4)2·8H2O and it is a dimorph of metaköttigite, which means that the two minerals have the same formula, but a different structure: köttigite is monoclinic and metaköttigite is triclinic. There are several minerals with similar formulae but with other cations in place of the zinc. Iron forms parasymplesite Fe2+3(AsO4)2·8H2O; cobalt forms the distinctively coloured pinkish purple mineral erythrite Co3(AsO4)2·8H2O and nickel forms annabergite Ni3(AsO4)2·8H2O. Köttigite forms series with all three of these minerals and they are all members of the vivianite group.

<span class="mw-page-title-main">Felsőbányaite</span>

Felsőbányaite or basaluminite is a hydrated aluminium sulfate mineral with formula: Al4(SO4)(OH)10·4H2O. It is a rare white to pale yellow mineral which typically occurs as globular masses and incrustations or as minute rhombic crystals. It crystallizes in the monoclinic crystal system.

<span class="mw-page-title-main">Sturmanite</span>

Sturmanite is a rare sulfate mineral with the chemical formula Ca6Fe3+2(SO4)2.5(B(OH)4)(OH)12 · 25 H2O. It crystallises in the tetragonal system and it has a Moh's hardness of 2.5. Sturmanite has a bright yellow to amber colour and falls in the ettringite group. It was named after Bozidar Darko Sturman (born 1937), Croatian-Canadian mineralogist and Curator Emeritus of Mineralogy, Royal Ontario Museum.

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