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VOOZH | about |
| Regional Level Types | |
|---|---|
| Playa de Enramada | Outcrop |
| Tenerife | Island |
| Santa Cruz de Tenerife Province | Province |
| Canary Islands | Group of Autonomous Communities |
| Spain | Country |
| Place | Population | Distance |
|---|---|---|
| Adeje | 43,204 (2012) | 3.7km |
| Playa de las Américas | 3,000 (2015) | 4.4km |
| Arona | 78,614 (2015) | 7.0km |
| Guía de Isora | 20,536 (2012) | 12.9km |
| Vilaflor | 1,981 (2012) | 13.1km |
| ⓘ Formula: LaSr(CO3)2(OH) · H2O Description: The paper doesn't inform about any analytical details that could confirm this identification.
The list of minerals is absolutely unbelievable and also impossible: numerous rare and ultra-rare species that are typical for completely different environments.
"Interesting": a lava flow that contains ultra-rare peralkaline/sodalitite pegmatites, LCT pegmatites, metamanganolites, and sedimentary vanadium deposits............. ? References: |
| ⓘ Formula: PbSO4 Description: The paper doesn't inform about any analytical details that could confirm this identification.
The list of minerals is absolutely unbelievable and also impossible: numerous rare and ultra-rare species that are typical for completely different environments.
"Interesting": a lava flow that contains ultra-rare peralkaline/sodalitite pegmatites, LCT pegmatites, metamanganolites, and sedimentary vanadium deposits............. ? References: |
| ⓘ 'Apatite' Formula: Ca5(PO4)3(Cl/F/OH) References: |
| ⓘ Formula: Be2Ba(Si2O7) Description: The paper doesn't inform about any analytical details that could confirm this identification.
The list of minerals is absolutely unbelievable and also impossible: numerous rare and ultra-rare species that are typical for completely different environments.
"Interesting": a lava flow that contains ultra-rare peralkaline/sodalitite pegmatites, LCT pegmatites, metamanganolites, and sedimentary vanadium deposits............. ? References: |
| ⓘ Bertrandite Formula: Be4(Si2O7)(OH)2 References: |
| ⓘ Formula: Mn3+2O3 Description: The paper doesn't inform about any analytical details that could confirm this identification.
The list of minerals is absolutely unbelievable and also impossible: numerous rare and ultra-rare species that are typical for completely different environments.
"Interesting": a lava flow that contains ultra-rare peralkaline/sodalitite pegmatites, LCT pegmatites, metamanganolites, and sedimentary vanadium deposits............. ? References: |
| ⓘ Formula: (Be,◻)(V3+,Ti,Cr)3O6 Description: The paper doesn't inform about any analytical details that could confirm this identification.
The list of minerals is absolutely unbelievable and also impossible: numerous rare and ultra-rare species that are typical for completely different environments.
"Interesting": a lava flow that contains ultra-rare peralkaline/sodalitite pegmatites, LCT pegmatites, metamanganolites, and sedimentary vanadium deposits............. ?
... and now an emerald deposit comes into ????????????? References: |
| ⓘ Formula: Mn2+3Si2O5(OH)4 Description: The paper doesn't inform about any analytical details that could confirm this identification.
The list of minerals is absolutely unbelievable and also impossible: numerous rare and ultra-rare species that are typical for completely different environments.
"Interesting": a lava flow that contains ultra-rare peralkaline/sodalitite pegmatites, LCT pegmatites, metamanganolites, and sedimentary vanadium deposits............. ? References: |
| ⓘ Formula: (Na2,K2,Ca,Sr,Mg)2[Al2Si4O12]2 · 12H2O Description: The paper doesn't inform about any analytical details that could confirm this identification.
The list of minerals is absolutely unbelievable and also impossible: numerous rare and ultra-rare species that are typical for completely different environments.
"Interesting": a lava flow that contains ultra-rare peralkaline/sodalitite pegmatites, LCT pegmatites, metamanganolites, and sedimentary vanadium deposits............. ? References: |
| ⓘ Formula: Ce4(Ti,Fe2+,Fe3+)5O8(Si2O7)2 Description: The paper doesn't inform about any analytical details that could confirm this identification.
The list of minerals is absolutely unbelievable and also impossible: numerous rare and ultra-rare species that are typical for completely different environments.
"Interesting": a lava flow that contains ultra-rare peralkaline/sodalitite pegmatites, LCT pegmatites, metamanganolites, and sedimentary vanadium deposits............. ? References: |
| ⓘ Formula: (LiAl4◻)[AlSi3O10](OH)8 Description: The paper doesn't inform about any analytical details that could confirm this identification.
The list of minerals is absolutely unbelievable and also impossible: numerous rare and ultra-rare species that are typical for completely different environments.
"Interesting": a lava flow that contains ultra-rare peralkaline/sodalitite pegmatites, LCT pegmatites, metamanganolites, and sedimentary vanadium deposits............. ? References: |
| ⓘ Formula: PbCl2 Description: The paper doesn't inform about any analytical details that could confirm this identification.
The list of minerals is absolutely unbelievable and also impossible: numerous rare and ultra-rare species that are typical for completely different environments.
"Interesting": a lava flow that contains ultra-rare peralkaline/sodalitite pegmatites, LCT pegmatites, metamanganolites, and sedimentary vanadium deposits............. ? References: |
| ⓘ Formula: Fe2+V3+2O4 Description: The paper doesn't inform about any analytical details that could confirm this identification.
The list of minerals is absolutely unbelievable and also impossible: numerous rare and ultra-rare species that are typical for completely different environments.
"Interesting": a lava flow that contains ultra-rare peralkaline/sodalitite pegmatites, LCT pegmatites, metamanganolites, and sedimentary vanadium deposits............. ? References: |
| ⓘ Formula: PbZn(VO4)(OH) Description: The paper doesn't inform about any analytical details that could confirm this identification.
The list of minerals is absolutely unbelievable and also impossible: numerous rare and ultra-rare species that are typical for completely different environments.
"Interesting": a lava flow that contains ultra-rare peralkaline/sodalitite pegmatites, LCT pegmatites, metamanganolites, and sedimentary vanadium deposits............. ? References: |
| ⓘ Formula: Na(Li1.5Al1.5)Al6(Si6O18)(BO3)3(OH)3(OH) Description: The paper doesn't inform about any analytical details that could confirm this identification.
The list of minerals is absolutely unbelievable and also impossible: numerous rare and ultra-rare species that are typical for completely different environments.
"Interesting": a lava flow that contains ultra-rare peralkaline/sodalitite pegmatites, LCT pegmatites, metamanganolites, and sedimentary vanadium deposits............. ?
Tourmalines in lava flows. Of course................. References: |
| ⓘ Formula: (Na◻)Nb2Na3Ti(Si2O7)2O2(OH)2(H2O)4 Description: The paper doesn't inform about any analytical details that could confirm this identification.
The list of minerals is absolutely unbelievable and also impossible: numerous rare and ultra-rare species that are typical for completely different environments.
"Interesting": a lava flow that contains ultra-rare peralkaline/sodalitite pegmatites, LCT pegmatites, metamanganolites, and sedimentary vanadium deposits............. ? References: |
| ⓘ Formula: Na15Ca6Fe3Zr3Si(Si25O73)(O,OH,H2O)3(Cl,OH)2 Description: The paper doesn't inform about any analytical details that could confirm this identification.
The list of minerals is absolutely unbelievable and also impossible: numerous rare and ultra-rare species that are typical for completely different environments.
"Interesting": a lava flow that contains ultra-rare peralkaline/sodalitite pegmatites, LCT pegmatites, metamanganolites, and sedimentary vanadium deposits............. ? References: |
| ⓘ Formula: YNbO4 Description: The paper doesn't inform about any analytical details that could confirm this identification.
The list of minerals is absolutely unbelievable and also impossible: numerous rare and ultra-rare species that are typical for completely different environments.
"Interesting": a lava flow that contains ultra-rare peralkaline/sodalitite pegmatites, LCT pegmatites, metamanganolites, and sedimentary vanadium deposits............. ? References: |
| ⓘ Formula: (Ca,K)(V5+,V4+,Fe2+)8O20 · 10H2O Description: The paper doesn't inform about any analytical details that could confirm this identification.
The list of minerals is absolutely unbelievable and also impossible: numerous rare and ultra-rare species that are typical for completely different environments.
"Interesting": a lava flow that contains ultra-rare peralkaline/sodalitite pegmatites, LCT pegmatites, metamanganolites, and sedimentary vanadium deposits............. ? References: |
| ⓘ Galena Formula: PbS References: |
| ⓘ Formula: Be2(BO3)(OH) Description: The paper doesn't inform about any analytical details that could confirm this identification.
The list of minerals is absolutely unbelievable and also impossible: numerous rare and ultra-rare species that are typical for completely different environments.
"Interesting": a lava flow that contains ultra-rare peralkaline/sodalitite pegmatites, LCT pegmatites, metamanganolites, and sedimentary vanadium deposits............. ? References: |
| ⓘ Formula: Mn2+Mn3+2O4 Description: The paper doesn't inform about any analytical details that could confirm this identification.
The list of minerals is absolutely unbelievable and also impossible: numerous rare and ultra-rare species that are typical for completely different environments.
"Interesting": a lava flow that contains ultra-rare peralkaline/sodalitite pegmatites, LCT pegmatites, metamanganolites, and sedimentary vanadium deposits............. ? References: |
| ⓘ Formula: Be3Mn2+4(SiO4)3S Description: The paper doesn't inform about any analytical details that could confirm this identification.
The list of minerals is absolutely unbelievable and also impossible: numerous rare and ultra-rare species that are typical for completely different environments.
"Interesting": a lava flow that contains ultra-rare peralkaline/sodalitite pegmatites, LCT pegmatites, metamanganolites, and sedimentary vanadium deposits............. ? References: |
| ⓘ Formula: (Na,Ca,K)6(Si,Al)36O72 · 22H2O Description: The paper doesn't inform about any analytical details that could confirm this identification.
The list of minerals is absolutely unbelievable and also impossible: numerous rare and ultra-rare species that are typical for completely different environments.
"Interesting": a lava flow that contains ultra-rare peralkaline/sodalitite pegmatites, LCT pegmatites, metamanganolites, and sedimentary vanadium deposits............. ? References: |
| ⓘ Formula: (Na,Ca)3(Mn2+,Fe2+)3(Ti,Zr,Nb)2(Si2O7)2O2(OH,F)2 Description: The paper doesn't inform about any analytical details that could confirm this identification.
The list of minerals is absolutely unbelievable and also impossible: numerous rare and ultra-rare species that are typical for completely different environments.
"Interesting": a lava flow that contains ultra-rare peralkaline/sodalitite pegmatites, LCT pegmatites, metamanganolites, and sedimentary vanadium deposits............. ? References: |
| ⓘ Formula: Na4K4(Ba,K)2Mg(Ti,Nb)8(Si4O12)4(O,OH)8 · 10H2O Description: The paper doesn't inform about any analytical details that could confirm this identification.
The list of minerals is absolutely unbelievable and also impossible: numerous rare and ultra-rare species that are typical for completely different environments.
"Interesting": a lava flow that contains ultra-rare peralkaline/sodalitite pegmatites, LCT pegmatites, metamanganolites, and sedimentary vanadium deposits............. ?
Or maybe labuntsovite-Ra ? References: |
| ⓘ Formula: Ca2NbFe3+O6 Description: The paper doesn't inform about any analytical details that could confirm this identification.
The list of minerals is absolutely unbelievable and also impossible: numerous rare and ultra-rare species that are typical for completely different environments.
"Interesting": a lava flow that contains ultra-rare peralkaline/sodalitite pegmatites, LCT pegmatites, metamanganolites, and sedimentary vanadium deposits............. ? References: |
| ⓘ Formula: (Na,REE)2Ti2O6 Description: The paper doesn't inform about any analytical details that could confirm this identification.
The list of minerals is absolutely unbelievable and also impossible: numerous rare and ultra-rare species that are typical for completely different environments.
"Interesting": a lava flow that contains ultra-rare peralkaline/sodalitite pegmatites, LCT pegmatites, metamanganolites, and sedimentary vanadium deposits............. ? References: |
| ⓘ Formula: CeTi2(O,OH)6 Description: The paper doesn't inform about any analytical details that could confirm this identification.
The list of minerals is absolutely unbelievable and also impossible: numerous rare and ultra-rare species that are typical for completely different environments.
"Interesting": a lava flow that contains ultra-rare peralkaline/sodalitite pegmatites, LCT pegmatites, metamanganolites, and sedimentary vanadium deposits............. ? References: |
| ⓘ Formula: NaNbO3 Description: The paper doesn't inform about any analytical details that could confirm this identification.
The list of minerals is absolutely unbelievable and also impossible: numerous rare and ultra-rare species that are typical for completely different environments.
"Interesting": a lava flow that contains ultra-rare peralkaline/sodalitite pegmatites, LCT pegmatites, metamanganolites, and sedimentary vanadium deposits............. ? References: |
| ⓘ Formula: Na2BeSi4O10 · 4H2O Description: The paper doesn't inform about any analytical details that could confirm this identification.
The list of minerals is absolutely unbelievable and also impossible: numerous rare and ultra-rare species that are typical for completely different environments.
"Interesting": a lava flow that contains ultra-rare peralkaline/sodalitite pegmatites, LCT pegmatites, metamanganolites, and sedimentary vanadium deposits............. ? References: |
| ⓘ Formula: (Na,◻)8Nb4(Si4O12)2(O,OH)4 · 8H2O Description: The paper doesn't inform about any analytical details that could confirm this identification.
The list of minerals is absolutely unbelievable and also impossible: numerous rare and ultra-rare species that are typical for completely different environments.
"Interesting": a lava flow that contains ultra-rare peralkaline/sodalitite pegmatites, LCT pegmatites, metamanganolites, and sedimentary vanadium deposits............. ? References: |
| ⓘ ' Formula: A2Nb2(O,OH)6Z Description: The paper doesn't inform about any analytical details that could confirm this identification.
The list of minerals is absolutely unbelievable and also impossible: numerous rare and ultra-rare species that are typical for completely different environments.
"Interesting": a lava flow that contains ultra-rare peralkaline/sodalitite pegmatites, LCT pegmatites, metamanganolites, and sedimentary vanadium deposits............. ? References: |
| ⓘ Formula: Na3CeSi6O15 · 2H2O Description: The paper doesn't inform about any analytical details that could confirm this identification.
The list of minerals is absolutely unbelievable and also impossible: numerous rare and ultra-rare species that are typical for completely different environments.
"Interesting": a lava flow that contains ultra-rare peralkaline/sodalitite pegmatites, LCT pegmatites, metamanganolites, and sedimentary vanadium deposits............. ? References: |
| ⓘ Formula: MgF2 Description: The paper doesn't inform about any analytical details that could confirm this identification.
The list of minerals is absolutely unbelievable and also impossible: numerous rare and ultra-rare species that are typical for completely different environments.
"Interesting": a lava flow that contains ultra-rare peralkaline/sodalitite pegmatites, LCT pegmatites, metamanganolites, and sedimentary vanadium deposits............. ? References: |
| ⓘ Formula: LiAlSi2O6 Description: The paper doesn't inform about any analytical details that could confirm this identification.
The list of minerals is absolutely unbelievable and also impossible: numerous rare and ultra-rare species that are typical for completely different environments.
"Interesting": a lava flow that contains ultra-rare peralkaline/sodalitite pegmatites, LCT pegmatites, metamanganolites, and sedimentary vanadium deposits............. ? References: |
| ⓘ Titanite Formula: CaTi(SiO4)O References: |
| ⓘ Formula: Ca3(Si3O9) Description: The paper doesn't inform about any analytical details that could confirm this identification.
The list of minerals is absolutely unbelievable and also impossible: numerous rare and ultra-rare species that are typical for completely different environments.
"Interesting": a lava flow that contains ultra-rare peralkaline/sodalitite pegmatites, LCT pegmatites, metamanganolites, and sedimentary vanadium deposits............. ? References: |
| ⓘ Xenotime-(Y) Formula: Y(PO4) References: |
| ⓘ Zircon Formula: Zr(SiO4) References: |
| ⓘ Formula: CaZrTi2O7 Description: The paper doesn't inform about any analytical details that could confirm this identification.
The list of minerals is absolutely unbelievable and also impossible: numerous rare and ultra-rare species that are typical for completely different environments.
"Interesting": a lava flow that contains ultra-rare peralkaline/sodalitite pegmatites, LCT pegmatites, metamanganolites, and sedimentary vanadium deposits............. ? References: |
| Group 2 - Sulphides and Sulfosalts | |||
|---|---|---|---|
| ⓘ | Galena | 2.CD.10 | PbS |
| Group 3 - Halides | |||
| ⓘ | Sellaite ? | 3.AB.15 | MgF2 |
| ⓘ | Cotunnite ? | 3.AB.85 | PbCl2 |
| Group 4 - Oxides and Hydroxides | |||
| ⓘ | 'Pyrochlore Group' ? | 4.00. | A2Nb2(O,OH)6Z |
| ⓘ | Coulsonite ? | 4.BB.05 | Fe2+V3+2O4 |
| ⓘ | Hausmannite ? | 4.BB.10 | Mn2+Mn3+2O4 |
| ⓘ | Byrudite ? | 4.CA. | (Be,◻)(V3+,Ti,Cr)3O6 |
| ⓘ | Bixbyite-(Mn) ? | 4.CB.10 | Mn3+2O3 |
| ⓘ | Latrappite ? | 4.CC.30 | Ca2NbFe3+O6 |
| ⓘ | Lueshite ? | 4.CC.30 | NaNbO3 |
| ⓘ | Loparite ? | 4.CC.35 | (Na,REE)2Ti2O6 |
| ⓘ | Lucasite-(Ce) ? | 4.DH.10 | CeTi2(O,OH)6 |
| ⓘ | Zirconolite ? | 4.DH.30 | CaZrTi2O7 |
| ⓘ | Fernandinite ? | 4.HE.20 | (Ca,K)(V5+,V4+,Fe2+)8O20 · 10H2O |
| Group 5 - Nitrates and Carbonates | |||
| ⓘ | Ancylite-(La) ? | 5.DC.05 | LaSr(CO3)2(OH) · H2O |
| Group 6 - Borates | |||
| ⓘ | Hambergite ? | 6.AB.05 | Be2(BO3)(OH) |
| Group 7 - Sulphates, Chromates, Molybdates and Tungstates | |||
| ⓘ | Anglesite ? | 7.AD.35 | PbSO4 |
| ⓘ | Fergusonite-(Y) ? | 7.GA.05 | YNbO4 |
| Group 8 - Phosphates, Arsenates and Vanadates | |||
| ⓘ | Xenotime-(Y) | 8.AD.35 | Y(PO4) |
| ⓘ | Descloizite ? | 8.BH.40 | PbZn(VO4)(OH) |
| Group 9 - Silicates | |||
| ⓘ | Zircon | 9.AD.30 | Zr(SiO4) |
| ⓘ | Titanite | 9.AG.15 | CaTi(SiO4)O |
| ⓘ | Barylite ? | 9.BB.15 | Be2Ba(Si2O7) |
| ⓘ | Bertrandite | 9.BD.05 | Be4(Si2O7)(OH)2 |
| ⓘ | Janhaugite ? | 9.BE.17 | (Na,Ca)3(Mn2+,Fe2+)3(Ti,Zr,Nb)2(Si2O7)2O2(OH,F)2 |
| ⓘ | Epistolite ? | 9.BE.30 | (Na◻)Nb2Na3Ti(Si2O7)2O2(OH)2(H2O)4 |
| ⓘ | Chevkinite-(Ce) ? | 9.BE.70 | Ce4(Ti,Fe2+,Fe3+)5O8(Si2O7)2 |
| ⓘ | Nenadkevichite ? | 9.CE.30a | (Na,◻)8Nb4(Si4O12)2(O,OH)4 · 8H2O |
| ⓘ | Labuntsovite-Mg ? | 9.CE.30e | Na4K4(Ba,K)2Mg(Ti,Nb)8(Si4O12)4(O,OH)8 · 10H2O |
| ⓘ | Elbaite ? | 9.CK.05 | Na(Li1.5Al1.5)Al6(Si6O18)(BO3)3(OH)3(OH) |
| ⓘ | Eudialyte ? | 9.CO.10 | Na15Ca6Fe3Zr3Si(Si25O73)(O,OH,H2O)3(Cl,OH)2 |
| ⓘ | Spodumene ? | 9.DA.30 | LiAlSi2O6 |
| ⓘ | Wollastonite ? | 9.DG.05 | Ca3(Si3O9) |
| ⓘ | Sazhinite-(Ce) ? | 9.EA.30 | Na3CeSi6O15 · 2H2O |
| ⓘ | Nabesite ? | 9.EA.65 | Na2BeSi4O10 · 4H2O |
| ⓘ | Cookeite ? | 9.EC.55 | (LiAl4◻)[AlSi3O10](OH)8 |
| ⓘ | Caryopilite ? | 9.ED.15 | Mn2+3Si2O5(OH)4 |
| ⓘ | Helvine ? | 9.FB.10 | Be3Mn2+4(SiO4)3S |
| ⓘ | Chabazite-Na ? | 9.GD.10 | (Na2,K2,Ca,Sr,Mg)2[Al2Si4O12]2 · 12H2O |
| ⓘ | Heulandite-Na ? | 9.GE.05 | (Na,Ca,K)6(Si,Al)36O72 · 22H2O |
| Unclassified | |||
| ⓘ | 'Apatite' | - | Ca5(PO4)3(Cl/F/OH) |
| H | Hydrogen | |
|---|---|---|
| H | ⓘ Bertrandite | Be4(Si2O7)(OH)2 |
| H | ⓘ Caryopilite | Mn32+Si2O5(OH)4 |
| H | ⓘ Cookeite | (LiAl4◻)[AlSi3O10](OH)8 |
| H | ⓘ Descloizite | PbZn(VO4)(OH) |
| H | ⓘ Elbaite | Na(Li1.5Al1.5)Al6(Si6O18)(BO3)3(OH)3(OH) |
| H | ⓘ Epistolite | (Na◻)Nb2Na3Ti(Si2O7)2O2(OH)2(H2O)4 |
| H | ⓘ Eudialyte | Na15Ca6Fe3Zr3Si(Si25O73)(O,OH,H2O)3(Cl,OH)2 |
| H | ⓘ Fernandinite | (Ca,K)(V5+,V4+,Fe2+)8O20 · 10H2O |
| H | ⓘ Hambergite | Be2(BO3)(OH) |
| H | ⓘ Janhaugite | (Na,Ca)3(Mn2+,Fe2+)3(Ti,Zr,Nb)2(Si2O7)2O2(OH,F)2 |
| H | ⓘ Lucasite-(Ce) | CeTi2(O,OH)6 |
| H | ⓘ Nenadkevichite | (Na,◻)8Nb4(Si4O12)2(O,OH)4 · 8H2O |
| H | ⓘ Pyrochlore Group | A2Nb2(O,OH)6Z |
| H | ⓘ Sazhinite-(Ce) | Na3CeSi6O15 · 2H2O |
| H | ⓘ Ancylite-(La) | LaSr(CO3)2(OH) · H2O |
| H | ⓘ Chabazite-Na | (Na2,K2,Ca,Sr,Mg)2[Al2Si4O12]2 · 12H2O |
| H | ⓘ Heulandite-Na | (Na,Ca,K)6(Si,Al)36O72 · 22H2O |
| H | ⓘ Labuntsovite-Mg | Na4K4(Ba,K)2Mg(Ti,Nb)8(Si4O12)4(O,OH)8 · 10H2O |
| H | ⓘ Nabesite | Na2BeSi4O10 · 4H2O |
| H | ⓘ Apatite | Ca5(PO4)3(Cl/F/OH) |
| Li | Lithium | |
| Li | ⓘ Cookeite | (LiAl4◻)[AlSi3O10](OH)8 |
| Li | ⓘ Elbaite | Na(Li1.5Al1.5)Al6(Si6O18)(BO3)3(OH)3(OH) |
| Li | ⓘ Spodumene | LiAlSi2O6 |
| Be | Beryllium | |
| Be | ⓘ Barylite | Be2Ba(Si2O7) |
| Be | ⓘ Bertrandite | Be4(Si2O7)(OH)2 |
| Be | ⓘ Hambergite | Be2(BO3)(OH) |
| Be | ⓘ Helvine | Be3Mn42+(SiO4)3S |
| Be | ⓘ Nabesite | Na2BeSi4O10 · 4H2O |
| Be | ⓘ Byrudite | (Be,◻)(V3+,Ti,Cr)3O6 |
| B | Boron | |
| B | ⓘ Elbaite | Na(Li1.5Al1.5)Al6(Si6O18)(BO3)3(OH)3(OH) |
| B | ⓘ Hambergite | Be2(BO3)(OH) |
| C | Carbon | |
| C | ⓘ Ancylite-(La) | LaSr(CO3)2(OH) · H2O |
| O | Oxygen | |
| O | ⓘ Anglesite | PbSO4 |
| O | ⓘ Barylite | Be2Ba(Si2O7) |
| O | ⓘ Bertrandite | Be4(Si2O7)(OH)2 |
| O | ⓘ Bixbyite-(Mn) | Mn23+O3 |
| O | ⓘ Caryopilite | Mn32+Si2O5(OH)4 |
| O | ⓘ Cookeite | (LiAl4◻)[AlSi3O10](OH)8 |
| O | ⓘ Coulsonite | Fe2+V23+O4 |
| O | ⓘ Descloizite | PbZn(VO4)(OH) |
| O | ⓘ Elbaite | Na(Li1.5Al1.5)Al6(Si6O18)(BO3)3(OH)3(OH) |
| O | ⓘ Epistolite | (Na◻)Nb2Na3Ti(Si2O7)2O2(OH)2(H2O)4 |
| O | ⓘ Eudialyte | Na15Ca6Fe3Zr3Si(Si25O73)(O,OH,H2O)3(Cl,OH)2 |
| O | ⓘ Fergusonite-(Y) | YNbO4 |
| O | ⓘ Fernandinite | (Ca,K)(V5+,V4+,Fe2+)8O20 · 10H2O |
| O | ⓘ Hambergite | Be2(BO3)(OH) |
| O | ⓘ Hausmannite | Mn2+Mn23+O4 |
| O | ⓘ Helvine | Be3Mn42+(SiO4)3S |
| O | ⓘ Janhaugite | (Na,Ca)3(Mn2+,Fe2+)3(Ti,Zr,Nb)2(Si2O7)2O2(OH,F)2 |
| O | ⓘ Latrappite | Ca2NbFe3+O6 |
| O | ⓘ Loparite | (Na,REE)2Ti2O6 |
| O | ⓘ Lucasite-(Ce) | CeTi2(O,OH)6 |
| O | ⓘ Lueshite | NaNbO3 |
| O | ⓘ Nenadkevichite | (Na,◻)8Nb4(Si4O12)2(O,OH)4 · 8H2O |
| O | ⓘ Pyrochlore Group | A2Nb2(O,OH)6Z |
| O | ⓘ Sazhinite-(Ce) | Na3CeSi6O15 · 2H2O |
| O | ⓘ Spodumene | LiAlSi2O6 |
| O | ⓘ Titanite | CaTi(SiO4)O |
| O | ⓘ Wollastonite | Ca3(Si3O9) |
| O | ⓘ Xenotime-(Y) | Y(PO4) |
| O | ⓘ Zircon | Zr(SiO4) |
| O | ⓘ Zirconolite | CaZrTi2O7 |
| O | ⓘ Ancylite-(La) | LaSr(CO3)2(OH) · H2O |
| O | ⓘ Chabazite-Na | (Na2,K2,Ca,Sr,Mg)2[Al2Si4O12]2 · 12H2O |
| O | ⓘ Chevkinite-(Ce) | Ce4(Ti,Fe2+,Fe3+)5O8(Si2O7)2 |
| O | ⓘ Heulandite-Na | (Na,Ca,K)6(Si,Al)36O72 · 22H2O |
| O | ⓘ Labuntsovite-Mg | Na4K4(Ba,K)2Mg(Ti,Nb)8(Si4O12)4(O,OH)8 · 10H2O |
| O | ⓘ Nabesite | Na2BeSi4O10 · 4H2O |
| O | ⓘ Apatite | Ca5(PO4)3(Cl/F/OH) |
| O | ⓘ Byrudite | (Be,◻)(V3+,Ti,Cr)3O6 |
| F | Fluorine | |
| F | ⓘ Janhaugite | (Na,Ca)3(Mn2+,Fe2+)3(Ti,Zr,Nb)2(Si2O7)2O2(OH,F)2 |
| F | ⓘ Sellaite | MgF2 |
| F | ⓘ Apatite | Ca5(PO4)3(Cl/F/OH) |
| Na | Sodium | |
| Na | ⓘ Elbaite | Na(Li1.5Al1.5)Al6(Si6O18)(BO3)3(OH)3(OH) |
| Na | ⓘ Epistolite | (Na◻)Nb2Na3Ti(Si2O7)2O2(OH)2(H2O)4 |
| Na | ⓘ Eudialyte | Na15Ca6Fe3Zr3Si(Si25O73)(O,OH,H2O)3(Cl,OH)2 |
| Na | ⓘ Janhaugite | (Na,Ca)3(Mn2+,Fe2+)3(Ti,Zr,Nb)2(Si2O7)2O2(OH,F)2 |
| Na | ⓘ Loparite | (Na,REE)2Ti2O6 |
| Na | ⓘ Lueshite | NaNbO3 |
| Na | ⓘ Nenadkevichite | (Na,◻)8Nb4(Si4O12)2(O,OH)4 · 8H2O |
| Na | ⓘ Sazhinite-(Ce) | Na3CeSi6O15 · 2H2O |
| Na | ⓘ Chabazite-Na | (Na2,K2,Ca,Sr,Mg)2[Al2Si4O12]2 · 12H2O |
| Na | ⓘ Heulandite-Na | (Na,Ca,K)6(Si,Al)36O72 · 22H2O |
| Na | ⓘ Labuntsovite-Mg | Na4K4(Ba,K)2Mg(Ti,Nb)8(Si4O12)4(O,OH)8 · 10H2O |
| Na | ⓘ Nabesite | Na2BeSi4O10 · 4H2O |
| Mg | Magnesium | |
| Mg | ⓘ Sellaite | MgF2 |
| Mg | ⓘ Chabazite-Na | (Na2,K2,Ca,Sr,Mg)2[Al2Si4O12]2 · 12H2O |
| Mg | ⓘ Labuntsovite-Mg | Na4K4(Ba,K)2Mg(Ti,Nb)8(Si4O12)4(O,OH)8 · 10H2O |
| Al | Aluminium | |
| Al | ⓘ Cookeite | (LiAl4◻)[AlSi3O10](OH)8 |
| Al | ⓘ Elbaite | Na(Li1.5Al1.5)Al6(Si6O18)(BO3)3(OH)3(OH) |
| Al | ⓘ Spodumene | LiAlSi2O6 |
| Al | ⓘ Chabazite-Na | (Na2,K2,Ca,Sr,Mg)2[Al2Si4O12]2 · 12H2O |
| Al | ⓘ Heulandite-Na | (Na,Ca,K)6(Si,Al)36O72 · 22H2O |
| Si | Silicon | |
| Si | ⓘ Barylite | Be2Ba(Si2O7) |
| Si | ⓘ Bertrandite | Be4(Si2O7)(OH)2 |
| Si | ⓘ Caryopilite | Mn32+Si2O5(OH)4 |
| Si | ⓘ Cookeite | (LiAl4◻)[AlSi3O10](OH)8 |
| Si | ⓘ Elbaite | Na(Li1.5Al1.5)Al6(Si6O18)(BO3)3(OH)3(OH) |
| Si | ⓘ Epistolite | (Na◻)Nb2Na3Ti(Si2O7)2O2(OH)2(H2O)4 |
| Si | ⓘ Eudialyte | Na15Ca6Fe3Zr3Si(Si25O73)(O,OH,H2O)3(Cl,OH)2 |
| Si | ⓘ Helvine | Be3Mn42+(SiO4)3S |
| Si | ⓘ Janhaugite | (Na,Ca)3(Mn2+,Fe2+)3(Ti,Zr,Nb)2(Si2O7)2O2(OH,F)2 |
| Si | ⓘ Nenadkevichite | (Na,◻)8Nb4(Si4O12)2(O,OH)4 · 8H2O |
| Si | ⓘ Sazhinite-(Ce) | Na3CeSi6O15 · 2H2O |
| Si | ⓘ Spodumene | LiAlSi2O6 |
| Si | ⓘ Titanite | CaTi(SiO4)O |
| Si | ⓘ Wollastonite | Ca3(Si3O9) |
| Si | ⓘ Zircon | Zr(SiO4) |
| Si | ⓘ Chabazite-Na | (Na2,K2,Ca,Sr,Mg)2[Al2Si4O12]2 · 12H2O |
| Si | ⓘ Chevkinite-(Ce) | Ce4(Ti,Fe2+,Fe3+)5O8(Si2O7)2 |
| Si | ⓘ Heulandite-Na | (Na,Ca,K)6(Si,Al)36O72 · 22H2O |
| Si | ⓘ Labuntsovite-Mg | Na4K4(Ba,K)2Mg(Ti,Nb)8(Si4O12)4(O,OH)8 · 10H2O |
| Si | ⓘ Nabesite | Na2BeSi4O10 · 4H2O |
| P | Phosphorus | |
| P | ⓘ Xenotime-(Y) | Y(PO4) |
| P | ⓘ Apatite | Ca5(PO4)3(Cl/F/OH) |
| S | Sulfur | |
| S | ⓘ Anglesite | PbSO4 |
| S | ⓘ Galena | PbS |
| S | ⓘ Helvine | Be3Mn42+(SiO4)3S |
| Cl | Chlorine | |
| Cl | ⓘ Cotunnite | PbCl2 |
| Cl | ⓘ Eudialyte | Na15Ca6Fe3Zr3Si(Si25O73)(O,OH,H2O)3(Cl,OH)2 |
| Cl | ⓘ Apatite | Ca5(PO4)3(Cl/F/OH) |
| K | Potassium | |
| K | ⓘ Fernandinite | (Ca,K)(V5+,V4+,Fe2+)8O20 · 10H2O |
| K | ⓘ Chabazite-Na | (Na2,K2,Ca,Sr,Mg)2[Al2Si4O12]2 · 12H2O |
| K | ⓘ Heulandite-Na | (Na,Ca,K)6(Si,Al)36O72 · 22H2O |
| K | ⓘ Labuntsovite-Mg | Na4K4(Ba,K)2Mg(Ti,Nb)8(Si4O12)4(O,OH)8 · 10H2O |
| Ca | Calcium | |
| Ca | ⓘ Eudialyte | Na15Ca6Fe3Zr3Si(Si25O73)(O,OH,H2O)3(Cl,OH)2 |
| Ca | ⓘ Fernandinite | (Ca,K)(V5+,V4+,Fe2+)8O20 · 10H2O |
| Ca | ⓘ Janhaugite | (Na,Ca)3(Mn2+,Fe2+)3(Ti,Zr,Nb)2(Si2O7)2O2(OH,F)2 |
| Ca | ⓘ Latrappite | Ca2NbFe3+O6 |
| Ca | ⓘ Titanite | CaTi(SiO4)O |
| Ca | ⓘ Wollastonite | Ca3(Si3O9) |
| Ca | ⓘ Zirconolite | CaZrTi2O7 |
| Ca | ⓘ Chabazite-Na | (Na2,K2,Ca,Sr,Mg)2[Al2Si4O12]2 · 12H2O |
| Ca | ⓘ Heulandite-Na | (Na,Ca,K)6(Si,Al)36O72 · 22H2O |
| Ca | ⓘ Apatite | Ca5(PO4)3(Cl/F/OH) |
| Ti | Titanium | |
| Ti | ⓘ Epistolite | (Na◻)Nb2Na3Ti(Si2O7)2O2(OH)2(H2O)4 |
| Ti | ⓘ Janhaugite | (Na,Ca)3(Mn2+,Fe2+)3(Ti,Zr,Nb)2(Si2O7)2O2(OH,F)2 |
| Ti | ⓘ Loparite | (Na,REE)2Ti2O6 |
| Ti | ⓘ Lucasite-(Ce) | CeTi2(O,OH)6 |
| Ti | ⓘ Titanite | CaTi(SiO4)O |
| Ti | ⓘ Zirconolite | CaZrTi2O7 |
| Ti | ⓘ Chevkinite-(Ce) | Ce4(Ti,Fe2+,Fe3+)5O8(Si2O7)2 |
| Ti | ⓘ Labuntsovite-Mg | Na4K4(Ba,K)2Mg(Ti,Nb)8(Si4O12)4(O,OH)8 · 10H2O |
| Ti | ⓘ Byrudite | (Be,◻)(V3+,Ti,Cr)3O6 |
| V | Vanadium | |
| V | ⓘ Coulsonite | Fe2+V23+O4 |
| V | ⓘ Descloizite | PbZn(VO4)(OH) |
| V | ⓘ Fernandinite | (Ca,K)(V5+,V4+,Fe2+)8O20 · 10H2O |
| V | ⓘ Byrudite | (Be,◻)(V3+,Ti,Cr)3O6 |
| Cr | Chromium | |
| Cr | ⓘ Byrudite | (Be,◻)(V3+,Ti,Cr)3O6 |
| Mn | Manganese | |
| Mn | ⓘ Bixbyite-(Mn) | Mn23+O3 |
| Mn | ⓘ Caryopilite | Mn32+Si2O5(OH)4 |
| Mn | ⓘ Hausmannite | Mn2+Mn23+O4 |
| Mn | ⓘ Helvine | Be3Mn42+(SiO4)3S |
| Mn | ⓘ Janhaugite | (Na,Ca)3(Mn2+,Fe2+)3(Ti,Zr,Nb)2(Si2O7)2O2(OH,F)2 |
| Fe | Iron | |
| Fe | ⓘ Coulsonite | Fe2+V23+O4 |
| Fe | ⓘ Eudialyte | Na15Ca6Fe3Zr3Si(Si25O73)(O,OH,H2O)3(Cl,OH)2 |
| Fe | ⓘ Fernandinite | (Ca,K)(V5+,V4+,Fe2+)8O20 · 10H2O |
| Fe | ⓘ Janhaugite | (Na,Ca)3(Mn2+,Fe2+)3(Ti,Zr,Nb)2(Si2O7)2O2(OH,F)2 |
| Fe | ⓘ Latrappite | Ca2NbFe3+O6 |
| Fe | ⓘ Chevkinite-(Ce) | Ce4(Ti,Fe2+,Fe3+)5O8(Si2O7)2 |
| Zn | Zinc | |
| Zn | ⓘ Descloizite | PbZn(VO4)(OH) |
| Sr | Strontium | |
| Sr | ⓘ Ancylite-(La) | LaSr(CO3)2(OH) · H2O |
| Sr | ⓘ Chabazite-Na | (Na2,K2,Ca,Sr,Mg)2[Al2Si4O12]2 · 12H2O |
| Y | Yttrium | |
| Y | ⓘ Fergusonite-(Y) | YNbO4 |
| Y | ⓘ Xenotime-(Y) | Y(PO4) |
| Zr | Zirconium | |
| Zr | ⓘ Eudialyte | Na15Ca6Fe3Zr3Si(Si25O73)(O,OH,H2O)3(Cl,OH)2 |
| Zr | ⓘ Janhaugite | (Na,Ca)3(Mn2+,Fe2+)3(Ti,Zr,Nb)2(Si2O7)2O2(OH,F)2 |
| Zr | ⓘ Zircon | Zr(SiO4) |
| Zr | ⓘ Zirconolite | CaZrTi2O7 |
| Nb | Niobium | |
| Nb | ⓘ Epistolite | (Na◻)Nb2Na3Ti(Si2O7)2O2(OH)2(H2O)4 |
| Nb | ⓘ Fergusonite-(Y) | YNbO4 |
| Nb | ⓘ Janhaugite | (Na,Ca)3(Mn2+,Fe2+)3(Ti,Zr,Nb)2(Si2O7)2O2(OH,F)2 |
| Nb | ⓘ Latrappite | Ca2NbFe3+O6 |
| Nb | ⓘ Lueshite | NaNbO3 |
| Nb | ⓘ Nenadkevichite | (Na,◻)8Nb4(Si4O12)2(O,OH)4 · 8H2O |
| Nb | ⓘ Pyrochlore Group | A2Nb2(O,OH)6Z |
| Nb | ⓘ Labuntsovite-Mg | Na4K4(Ba,K)2Mg(Ti,Nb)8(Si4O12)4(O,OH)8 · 10H2O |
| Ba | Barium | |
| Ba | ⓘ Barylite | Be2Ba(Si2O7) |
| Ba | ⓘ Labuntsovite-Mg | Na4K4(Ba,K)2Mg(Ti,Nb)8(Si4O12)4(O,OH)8 · 10H2O |
| La | Lanthanum | |
| La | ⓘ Ancylite-(La) | LaSr(CO3)2(OH) · H2O |
| Ce | Cerium | |
| Ce | ⓘ Lucasite-(Ce) | CeTi2(O,OH)6 |
| Ce | ⓘ Sazhinite-(Ce) | Na3CeSi6O15 · 2H2O |
| Ce | ⓘ Chevkinite-(Ce) | Ce4(Ti,Fe2+,Fe3+)5O8(Si2O7)2 |
| Pb | Lead | |
| Pb | ⓘ Anglesite | PbSO4 |
| Pb | ⓘ Cotunnite | PbCl2 |
| Pb | ⓘ Descloizite | PbZn(VO4)(OH) |
| Pb | ⓘ Galena | PbS |