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.
Abbreviations:
"*" – discredited (IMA/CNMNC status).
"?" – questionable/doubtful (IMA/CNMNC, mindat.org or mineralienatlas.de status).
N – published without approval of the IMA/CNMNC.
I – intermediate member of a solid-solution series.
H – hypothetical mineral (synthetic, anthropogenic, etc.)
ch – incomplete description, hypothetical solid solution end member.
group – a name used to designate a group of species, sometimes only a mineral group name.
no – no link available.
red. – redefinition of ...
Y: 1NNN – year of publication.
Y: old – known before publications were available.
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.
ClinotyroliteN (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]
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]
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]
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+xS ()), 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.
(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]
Nomenclature change: antimonpearceite was replaced by polybasite-Tac, arsenpolybasite-221 by pearceite-T2ac, arsenpolybasite-222 by pearceite-M2a2b2c, polybasite-221 by polybasite-T2ac, and polybasite-222 by polybasite-M2a2b2c.[53]
Douglas S. Coombs; Alberto Alberti; Thomas Armbruster; Gilberto Artioli; Carmine Colella; Ermanno Galli; Joel D. Grice; Friedrich Liebau; Joseph A. Mandarino; Hideo Minato; Ernest H. Nickel; Elio Passaglia; Donald R. Peacor; Simona Quartieri; Romano Rinaldi; Malcolm I. Ross; Richard A. Sheppard; Ekkehart Tillmanns & Giovanna Vezzalini (December 1997). "Recommended nomenclature for zeolite minerals: report of the subcommittee on zeolites of the international mineralogical association, commission on new minerals and mineral names". The Canadian Mineralogist. 35: 1571–1606.
"Subcommittee on amphiboles of the IMA/CNMNC"
Leake, Bernard E. (November 1978). "Nomenclature of amphiboles". The Canadian Mineralogist. 16: 501–520.
Hawthorne, Frank C. (May 1983). "The crystal chemistry of the amphiboles". The Canadian Mineralogist. 21 (2): 173–480.
Joseph A. Mandarino (1998). "The Second List of Additions and Corrections to the Glossary of Mineral Species (1995): The Amphibole Group". The Mineralogical Record. 29 (3): 169–174.
Bernard E. Leake; Alan R. Woolley; Charles E. S. Arps; William D. Birch; M. Charles Gilbert; Joel D. Grice; Frank C. Hawthorne; Akira Kato; Hanan J. Kisch; Vladimir G. Krivovichev; Kees Linthout; Jo Laird; Joseph A. Mandarino; Walter V. Maresch; Ernest H. Nickel; Nicholas M. S. Rock; John C. Schumacher; David C. Smith; Nick C. N. Stephenson; Luciano Ungaretti; Eric J. W. Whittaker & Guo Youzhi (February 1997). "Nomenclature of amphiboles: Report of the subcommittee on amphiboles of the International Mineralogical Association, commission on new minerals and mineral names". The Canadian Mineralogist. 35: 219–246.
Bernard E. Leake; Alan R. Woolley; William D. Birch; Ernst A.J. Burke; Giovanni Ferraris; Joel D. Grice; Frank C. Hawthorne; Hanan J. Kisch; Vladimir G. Krivovichev; John C. Schumacher; Nicholas C.N. Stephenson & Eric J.W. Whittaker (December 2003). "Nomenclature of amphiboles: additions and revisions to the International Mineralogical Association's 1997 recommendations". The Canadian Mineralogist. 41 (6): 1355–1362. Bibcode:2003CaMin..41.1355L. doi:10.2113/gscanmin.41.6.1355.
Burke, Ernst A.J.; Leake, Bernard E. (December 2004). "Named amphiboles: A new category of amphiboles recognized by the International Mineralogical Association (IMA), and the proper order of prefixes to be used in amphibole names". The Canadian Mineralogist. 42 (6): 1881–1884. Bibcode:2004CaMin..42.1881B. CiteSeerX10.1.1.549.4442. doi:10.2113/gscanmin.42.6.1881.
Bernard E. Leake; Alan R. Woolley; William D. Birch; Ernst A.J. Burke; Giovanni Ferraris; Joel D. Grice; Frank C. Hawthorne; Hanan J. Kisch; Vladimir G. Krivovichev; John C. Schumacher; Nicholas C.N. Stephenson & Eric J.W. Whittaker (2004). "Nomenclature of amphiboles: additions and revisions to the International Mineralogical Association's amphibole nomenclature". American Mineralogist. 89 (5–6): 883–887.
Frank C. Hawthorne; Roberta Oberti; George E. Harlow; Walter V. Maresch; Robert F. Martin; John C. Schumacher; Mark D. Welch (2012). "Nomenclature of the amphibole supergroup". American Mineralogist. 97 (11–12): 2031–2048. Bibcode:2012AmMin..97.2031H. doi:10.2138/am.2012.4276.
^Cooke, Edward I.; Cooke, Richard W.I.; Gardner, William, eds. (2019). Handbook of Chemical Synonyms and Trade Names. CRC Press. p. 61. ISBN978-1-351-08133-7.
^Lee, Yongjae, Hriljac, Joseph A., Parise, John B., and Vogt, Thomas (2006) Pressure-induced hydration in zeolite tetranatrolite. American Mineralogist: 91: 247-251.
^Seryotkin, Yu, V. & Bakakin, V.V. (2007) The reversibility of the paranatrolite-tetranatrolite transformation. European Journal of Mineralogy, 19, 593-598.
^Burns RG, Burns VE, Stockman HW (1983). "A review of the todorokite-buserite problem: implications to the mineralogy of marine manganese nodules". American Mineralogist. 68: 972–980.
^David Rickard; A. Griffith; A. Oldroyd; I.B. Butler; E. Lopez-Capel; D.A.C. Manning; D.C. Apperley (15 December 2006). "The composition of nanoparticulate mackinawite, tetragonal iron(II) monosulfide". Chemical Geology. 235 (3–4): 286–298. Bibcode:2006ChGeo.235..286R. doi:10.1016/j.chemgeo.2006.07.004.
^Topa, D.; Makovicky, E. (2010). "The crystal chemistry of cosalite based on new electron-microprobe data and single-crystal determinations of the structure". The Canadian Mineralogist. 48 (5): 1081–1107. Bibcode:2010CaMin..48.1081T. doi:10.3749/canmin.48.5.1081.
^Moëlo Y, Makovicky E, Mozgova NN, Jambor JL, Cook N, Pring A, Paar W, Nickel EH, Graeser S, Karup-Møller S, Balic-Zunic T, Mumme WG, Vurro F, Topa D, Bindi L, Bente K, Shimizu M (2008). "Sulfosalt systematics: a review. Report of the sulfosalt sub-committee of the IMA Commission on Ore Mineralogy". European Journal of Mineralogy. 20 (1): 7–46. Bibcode:2008EJMin..20....7M. doi:10.1127/0935-1221/2008/0020-1778.
^V. Mladenova, U. Kolitsch, T. Kenkman, L. Hecht and R.-T. Schmitt (2010): Reinvestigation of the type material of orpheite: is it a valid mineral species? Poster, 20th General Meeting of the IMA (IMA2010), Budapest, Hungary, August 21–27; abstract in CD of Abstracts, p. 498
^Bindi, L; Evain M; Spry P G; Menchetti S (2007). "The pearceite-polybasite group of minerals: crystal chemistry and new nomenclature rules". American Mineralogist. 92 (5–6): 918–925. Bibcode:2007AmMin..92..918B. doi:10.2138/am.2007.2440. S2CID54853946.
^Grice J D, Pring A (2012) Veatchite: structural relationships of the three polytypes, American Mineralogist 97, 489-495
^Back, Malcolm E. (2014). Fleischer's Glossary of Mineral Species (11 ed.). Tucson AZ: Mineralogical Record Inc. p. 434.