Bradleyite (original) (raw)
A valid IMA mineral species - grandfathered
About BradleyiteHide
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Crystal System:
Monoclinic
Name:
Named in 1941 by John Joseph Fahey in honor of geologist Wilmot Hyde Bradley [April 4, 1899 Westville, Connecticut, USA - April 12, 1979 Pigeon Hill Road, Bangor, Maine, USA], Chief Geologist of U.S. Geological Survey, who conducted geologic investigations in the Green River area, Wyoming. Bradley was a co-founder and Chief of the Branch of Military Geology in 1943 and was Chief Geologist of the United States Geological Survey from 1944 to 1959 and retired from the U. S. Geological Survey in 1970.
Structurally related to bonshtedtite.
May occur as fluid inclusions in chromite (Potapov et al., 2022).
Unique IdentifiersHide
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Long-form identifier:
mindat:1:1:750:4
c6f316aa-0d6e-4f84-8329-27d5e0a3c4f2
IMA Classification of BradleyiteHide
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Approved, 'Grandfathered' (first described prior to 1959)
IMA Formula:
Na3Mg(PO4)(CO3)
Type description reference:
Classification of BradleyiteHide
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5.BF.10
5 : CARBONATES (NITRATES)
B : Carbonates with additional anions, without H2O
F : With (Cl), SO4, PO4, TeO3
43.2.1.1
43 : COMPOUND PHOSPHATES, ETC.
2 : Anhydrous Normal Compound Phosphates, etc·
22.4.1
22 : Phosphates, Arsenates or Vanadates with other Anions
4 : Phosphates, arsenates or vanadates with carbonate
Mineral SymbolsHide
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As of 2021 there are now IMA–CNMNC approved mineral symbols (abbreviations) for each mineral species, useful for tables and diagrams.
Symbol | Source | Reference |
---|---|---|
Bd | IMA–CNMNC | Warr, L.N. (2021). IMA–CNMNC approved mineral symbols. Mineralogical Magazine, 85(3), 291-320. doi:10.1180/mgm.2021.43 |
Physical Properties of BradleyiteHide
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Density:
2.734 g/cm3 (Measured) 2.72 g/cm3 (Calculated)
Optical Data of BradleyiteHide
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RI values:
_n_α = 1.487(2) _n_β = 1.546(2) _n_γ = 1.560(2)
2V:
Measured: 49° , Calculated: 50°
δ = 0.073
Image shows birefringence interference colour range (at 30µm thickness)
and does not take into account mineral colouration.
Chemistry of BradleyiteHide
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Mindat Formula:
Na3Mg(CO3)(PO4)
Crystallography of BradleyiteHide
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Crystal System:
Monoclinic
Class (H-M):
2/m - Prismatic
Cell Parameters:
a = 8.85(1) Å, b = 6.63(1) Å, c = 5.16(1) Å
β = 90.42(5)°
Ratio:
a:b:c = 1.335 : 1 : 0.778
Unit Cell V:
302.76 ų (Calculated from Unit Cell)
Morphology:
Extremely fine-grained masses.
X-Ray Powder DiffractionHide
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Powder Diffraction Data:
d-spacing | Intensity |
---|---|
2.655 Å | (100) |
3.312 Å | (71) |
8.85 Å | (50) |
2.576 Å | (35) |
1.839 Å | (30) |
3.694 Å | (25) |
1.658 Å | (25) |
Geological EnvironmentHide
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Type Occurrence of BradleyiteHide
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General Appearance of Type Material:
extremely fine-grained masses.
Place of Conservation of Type Material:
National Museum of Natural History, Washington, D.C., USA, 117718.
Geological Setting of Type Material:
Associated Minerals at Type Locality:
Reference:
Fahey, J.J., Tunell, G. (1941) Bradleyite, a new mineral, sodium phosphate-magnesium carbonate. American Mineralogist: 26: 646-650.
Other Language Names for BradleyiteHide
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Common AssociatesHide
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Associated Minerals Based on Photo Data:
Related Minerals - Strunz-mindat GroupingHide
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5.BF.05 | Northupite | Na3Mg(CO3)2Cl | Iso. m_3(2/m_3) : F _d_3 |
---|---|---|---|
5.BF.05 | Manganotychite | Na6Mn2(CO3)4(SO4) | Iso. m_3(2/m_3) : F _d_3 |
5.BF.05 | Tychite | Na6Mg2(CO3)4(SO4) | Iso. m_3(2/m_3) : F _d_3 |
5.BF.05 | Ferrotychite | Na6(Fe,Mn,Mg)2(CO3)4(SO4) | Iso. m_3(2/m_3) : F _d_3 |
5.BF.10 | Sidorenkite | Na3Mn2+(CO3)(PO4) | Mon. |
5.BF.10 | Crawfordite | Na3Sr(CO3)(PO4) | Mon. 2 : _P_21 |
5.BF.10 | Bonshtedtite | Na3Fe2+(CO3)(PO4) | Mon. 2/m : _P_21/m |
5.BF.15 | Daqingshanite-(Ce) | (Sr,Ca,Ba)3(Ce,La)(CO3)3-x(PO4)(OH,F)2x | Trig. |
5.BF.20 | Reederite-(Y) | (Na,Mn)15Y2(CO3)9(FSO3)Cl | Hex. 6 : _P_6 |
5.BF.25 | Mineevite-(Y) | Na25Ba(Y,Gd,Dy)2(CO3)11(HCO3)4(SO4)2F2Cl | Hex. 6/m : _P_63/m |
5.BF.30 | Brianyoungite | Zn3(CO3,SO4)(OH)4 | Mon. 2/m : _P_21/m |
5.BF.35 | Philolithite | Pb12Mn2+(Mg,Mn2+)2(Mn2+,Mg)4(CO3)4(SO4)O6(OH)12Cl4 | Tet. 4/m m m _(_4/_m_2/_m_2/m ) |
5.BF.40 | Leadhillite | Pb4(CO3)2(SO4)(OH)2 | Mon. 2/m : _P_21/b |
5.BF.40 | Macphersonite | Pb4(CO3)2(SO4)(OH)2 | Orth. m m m _(_2/_m_2/_m_2/m ) |
5.BF.40 | Susannite | Pb4(CO3)2(SO4)(OH)2 | Trig. 3 : _P_3 |
5.BF.45 | Peatite-(Y) | Li4Na12Y12(PO4)12(CO3)4(F,OH)8 | Orth. 222 : _P_222 |
5.BF.50 | Ramikite-(Y) | Li4(Na,Ca)12Y6Zr6(PO4)12(CO3)4O4[(OH),F]4 | Tric. 1 : _P_1 |
Other InformationHide
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Notes:
Slowly decomposed by cold water with Na2CO3 released to solution. Readily soluble in dilute HCl.
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 BradleyiteHide
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References for BradleyiteHide
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Reference List:
Kozlov, Evgeniy Nikolaevich, Fomina, Ekaterina Nikolaevna, Bocharov, Vladimir Nikolaevich, Sidorov, Mikhail Yurievich, Vlasenko, Natalia Sergeevna, Shilovskikh, Vladimir Vladimirovich (2021) A Raman spectroscopic study of the natural carbonophosphates Na3_M_CO3PO4 (M is Mn, Fe, and Mg) European Journal of Mineralogy, 33 (3) 283-297 doi:10.5194/ejm-33-283-2021
Localities for BradleyiteHide
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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
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- 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.