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Johnbaumite-M

A discredited species name
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About Johnbaumite-MHide

Formula:
Ca5(AsO4)3OH
Colour:
White to light pink
Lustre:
Greasy
Hardness:
5
Specific Gravity:
3.518
Crystal System:
Monoclinic
Dimorph of:
Apatite Supergroup.
The arsenate analogue and monoclinic polymorph of hydroxylapatite.

Previously called 'fermorite', this mineral was reclassified as the monoclinic polymorph of Johnbaumite by Pasero et al. (2010), and is no longer regarded as a distinct mineral species.


Note: The orginal chemical analysis (from 1911) gave (PO4)1.60(AsO4)1.24, making fermorite a phosphate. A modern microprobe analysis of the type material, however, gave (PO4)1.45(AsO4)1.48 - thus this mineral is now defined as an arsenate.


Unique IdentifiersHide

Mindat ID:
1482
Long-form identifier:
mindat:1:1:1482:9
GUID
(UUID V4):
63cccf4e-b009-4ac6-a468-7275c29141a0

IMA Classification of Johnbaumite-MHide

Discredited

Classification of Johnbaumite-MHide

8.BN.05

8 : PHOSPHATES, ARSENATES, VANADATES
B : Phosphates, etc., with additional anions, without H2O
N : With only large cations, (OH, etc.):RO4 = 0.33:1
41.8.3.4

41 : ANHYDROUS PHOSPHATES, ETC.CONTAINING HYDROXYL OR HALOGEN
8 : A5(XO4)3Zq
22.1.30

22 : Phosphates, Arsenates or Vanadates with other Anions
1 : Phosphates, arsenates or vanadates with fluoride

Physical Properties of Johnbaumite-MHide

Greasy
Transparency:
Translucent
Colour:
White to light pink
Streak:
White
Hardness:
Fracture:
Irregular/Uneven
Density:
3.518 g/cm3 (Measured)    3.41 g/cm3 (Calculated)

Optical Data of Johnbaumite-MHide

Type:
Uniaxial (-)
RI values:
nω = 1.660 nε = 1.655
Max Birefringence:
δ = 0.005
Image shows birefringence interference colour range (at 30µm thickness)
and does not take into account mineral colouration.
Surface Relief:
Moderate

Chemistry of Johnbaumite-MHide

Mindat Formula:
Ca5(AsO4)3OH

Crystallography of Johnbaumite-MHide

Crystal System:
Monoclinic
Class (H-M):
2/m - Prismatic
Space Group:
P21/m
Cell Parameters:
a = 9.55 Å, c = 6.98 Å
Ratio:
a:c = 1 : 0.731
Unit Cell V:
0.00 ų (Calculated from Unit Cell)
Z:
2
Morphology:
Crystals crudely prismatic; massive, granular.
Comment:
Pseudohexagonal

First Recorded Occurrence of Johnbaumite-MHide

Place of Conservation of First Recorded Material:
Smithsonian 94809
Geological Setting of First Recorded Material:
Manganese deposit

Synonyms of Johnbaumite-MHide

Other Language Names for Johnbaumite-MHide

Simplified Chinese:锶磷灰石
Spanish:Fermorita
Traditional Chinese:鍶磷灰石

Related Minerals - Strunz-mindat GroupingHide

8.BN.AraditeBaCa6[(SiO4)(VO4)](VO4)2FTrig. 3m : R3m
8.BN.MagganasiteCuFe3+3O(AsO4)3Tric. 1 : P1
8.BN.FluorpyromorphitePb5(PO4)3FHex. 6/m : P63/m
8.BN.FluorsigaiiteCa2Sr3(PO4)3FHex. 6/m : P63/m
8.BN.FluoralforsiteBa5(PO4)3FHex. 6/m : P6/m
8.BN.05AlforsiteBa5(PO4)3ClHex. 6/m : P63/m
8.BN.05Belovite-(Ce)NaCeSr3(PO4)3FTrig. 3 : P3
8.BN.05ChlorapatiteCa5(PO4)3ClHex. 6/m : P63/m
8.BN.05Mimetite-MPb5(AsO4)3ClMon. 2/m : P21/b
8.BN.05FluorapatiteCa5(PO4)3FHex. 6/m : P63/m
8.BN.05HedyphaneCa2Pb3(AsO4)3ClHex. 6/mmm (6/m 2/m 2/m) : P63/mmc
8.BN.05HydroxylapatiteCa5(PO4)3(OH)Hex. 6/m : P63/m
8.BN.05JohnbaumiteCa5(AsO4)3(OH)Hex. 6/m : P63/m
8.BN.05MimetitePb5(AsO4)3ClHex. 6/m : P63/m
8.BN.05MorelanditeCa2Ba3(AsO4)3ClHex.
8.BN.05OxypyromorphitePb10(PO4)6O
8.BN.05PyromorphitePb5(PO4)3ClHex. 6/m : P63/m
8.BN.05FluorstrophiteSrCaSr3(PO4)3FHex. 6/m : P63/m
8.BN.05SvabiteCa5(AsO4)3FHex. 6/mmm (6/m 2/m 2/m) : P63/mmc
8.BN.05TurneaureiteCa5(AsO4)3ClHex. 6/m : P63/m
8.BN.05VanadinitePb5(VO4)3ClHex. 6/m : P63/m
8.BN.05Belovite-(La)NaLaSr3(PO4)3FTrig. 3 : P3
8.BN.05Deloneite(Na0.5REE0.25Ca0.25)(Ca0.75REE0.25)Sr1.5(CaNa0.25REE0.25)(PO4)3F0.5(OH)0.5Trig. 3 : P3
8.BN.05FluorcaphiteSrCaCa3(PO4)3FHex. 6/m : P63/m
8.BN.05 vaGermanate-pyromorphitePb5(PO4)2GeO4
8.BN.05Kuannersuite-(Ce)NaCeBa3(PO4)3F0.5Cl0.5Trig. 3 : P3
8.BN.05Hydroxylapatite-MCa5(PO4)3OHMon. 2/m : P21/b
8.BN.05PhosphohedyphaneCa2Pb3(PO4)3ClHex. 6/m : P63/m
8.BN.05HydroxylpyromorphitePb5(PO4)3(OH)Hex. 6/mmm (6/m 2/m 2/m) : P63/mcm
8.BN.05StronadelphiteSr5(PO4)3FHex. 6/m : P63/m
8.BN.05FluorphosphohedyphaneCa2Pb3(PO4)3FHex. 6/m : P63/m
8.BN.05Carlgieseckeite-(Nd)NaNdCa3(PO4)3FTrig. 3 : P3
8.BN.05VanackeritePb4Cd(AsO4)3ClTrig. 3 : P3
8.BN.05Miyahisaite(Sr,Ca)2Ba3(PO4)3F Hex. 6/m : P63/m
8.BN.05Unnamed (OH-analogue of Mimetite)Pb5(AsO4)3(OH)Hex. 6/m : P63/m
8.BN.05PieczkaiteMn5(PO4)3ClHex. 6/m : P63/m
8.BN.05HydroxylhedyphaneCa2Pb3(AsO4)3(OH)Trig. 3 : P3
8.BN.05PliniusiteCa5(VO4)3FHex. 6/m : P63/m
8.BN.05ParafiniukiteCa2Mn3(PO4)3ClHex. 6/m : P63/m
8.BN.10ArctiteNa2Ca4(PO4)3FTrig. 3m (3 2/m) : R3m
8.BN.15GoryainoviteCa2(PO4)ClOrth. mmm (2/m 2/m 2/m) : Pbcm

Fluorescence of Johnbaumite-MHide

Fluoresces bright orange to yellow orange in SWUV

Other InformationHide

Notes:
Soluble in acids.
Health Risks:
No information on health risks for this material has been entered into the database. You should always treat mineral specimens with care.

Internet Links for Johnbaumite-MHide

References for Johnbaumite-MHide

Reference List:

Localities for Johnbaumite-MHide

This map shows a selection of localities that have latitude and longitude coordinates recorded. Click on the symbol to view information about a locality. The symbol next to localities in the list can be used to jump to that position on the map.

Locality ListHide

- This locality has map coordinates listed. - This locality has estimated coordinates. ⓘ - Click for references and further information on this occurrence. ? - Indicates mineral may be doubtful at this locality. - Good crystals or important locality for species. - World class for species or very significant. (TL) - Type Locality for a valid mineral species. (FRL) - First Recorded Locality for everything else (eg varieties). Struck out - Mineral was erroneously reported from this locality. Faded * - Never found at this locality but inferred to have existed at some point in the past (e.g. from pseudomorphs).

All localities listed without proper references should be considered as questionable.
India (FRL)
 
  • Madhya Pradesh
    • Jabalpur Division
      • Chhindwara District
 
矿物 and/or 产地  
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