Bredigite (original) (raw)
A valid IMA mineral species - grandfathered
About BredigiteHide
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Crystal System:
Orthorhombic
Name:
Named in honor of Dr. Max Albrecht Bredig (20 June 1902 - 21 November 1977), physical chemist, who studied the polymorphism of Ca2SiO4. Dr. Bredig was former Associate Director of the Chemistry Division Oak Ridge National Laboratory, and expert in the chemistry of molten salts and chemistry of the solid state, especially high temperature and crystal chemistry.
Anthropogenic "Ca7MgSi4O16" is described by Žáček et al. (2005).
Unique IdentifiersHide
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Long-form identifier:
mindat:1:1:762:9
eae67ac7-9ef6-454f-aa1b-b86358da0271
IMA Classification of BredigiteHide
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Approved, 'Grandfathered' (first described prior to 1959)
Type description reference:
Classification of BredigiteHide
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9.AD.20
9 : SILICATES (Germanates)
A : Nesosilicates
D : Nesosilicates without additional anions; cations in [6] and/or greater coordination
51.4.1.1
51 : NESOSILICATES Insular SiO4 Groups Only
4 : Insular SiO4 Groups Only with cations in [6] and >[6] coordination
14.5.7
14 : Silicates not Containing Aluminum
5 : Silicates of Ca
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 |
---|---|---|
Bdi | 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 BredigiteHide
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Cleavage:
Distinct/Good
Distinct on {130}
Density:
3.42 g/cm3 (Measured) 3.32 g/cm3 (Calculated)
Optical Data of BredigiteHide
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RI values:
_n_α = 1.712 _n_β = 1.716 _n_γ = 1.725
2V:
Measured: 30° , Calculated: 68°
δ = 0.013
Image shows birefringence interference colour range (at 30µm thickness)
and does not take into account mineral colouration.
Dispersion:
relatively strong
Comments:
In thick sections, X = pale violet; Y = Z = colorless to pale green. X=b, Y=a, Z=c.
Chemistry of BredigiteHide
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Mindat Formula:
Ca7Mg(SiO4)4
Common Impurities:
Ti,Fe,Mn,Ba,F
Crystallography of BredigiteHide
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Crystal System:
Orthorhombic
Class (H-M):
m _m_2 - Pyramidal
Cell Parameters:
a = 10.909(9) Å, b = 18.34(1) Å, c = 6.739(9) Å
Ratio:
a:b:c = 0.595 : 1 : 0.367
Unit Cell V:
1,348.28 ų (Calculated from Unit Cell)
Twinning:
Simple contact and cyclical on {110}.
Crystal StructureHide
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ID | Species | Reference | Link | Year | Locality | Pressure (GPa) | Temp (K) |
---|---|---|---|---|---|---|---|
0000494 | Bredigite | Moore P B, Araki T (1976) The crystal structure of bredigite and the genealogy of some alkaline earth orthosilicates American Mineralogist 61 74-87 | ![]() |
1976 | 0 | 293 |
CIF Raw Data - click here to close
X-Ray Powder DiffractionHide
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Powder Diffraction Data:
d-spacing | Intensity |
---|---|
2.730 Å | (100) |
2.663 Å | (100) |
2.259 Å | (80) |
1.923 Å | (80) |
2.067 Å | (60) |
1.574 Å | (60) |
1.554 Å | (60) |
Geological EnvironmentHide
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Type Occurrence of BredigiteHide
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General Appearance of Type Material:
Crystals are squat, barrel- or boat-shaped, with pseudohexagonal cross sections, or as slender prismatic crystals, to 2mm
Place of Conservation of Type Material:
The Natural History Museum, London, England, 1956, 385.
Geological Setting of Type Material:
Type specimen was from slag (Middlesbrough type specimen of Tilley and Vincent)
Associated Minerals at Type Locality:
Reference:
Tilley, C.E., Vincent, C.G. (1948) The occurrence of an orthorhombic high temperature form of Ca2SiO4 (bredigite) in the Scawt Hill contact-zone and as a constituent of slags. Mineralogical Magazine: 28: 255-271.
Other Language Names for BredigiteHide
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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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9.AD. | Adrianite | Ca12(Al4Mg3Si7)O32Cl6 | Iso. 43_m_ : I_43_d |
---|---|---|---|
9.AD.05 | Larnite | Ca2SiO4 | Mon. 2/m |
9.AD.10 | Calcio-olivine | Ca2SiO4 | Orth. m m m _(_2/_m_2/_m_2/m ) |
9.AD.15 | Merwinite | Ca3Mg(SiO4)2 | Mon. 2/m : _P_21/b |
9.AD.25 | Midbarite | Ca3Mg2(V2Si)O12 | Iso. m_3_m _(_4/_m_32/m ) |
9.AD.25 | Menzerite-(Y) | (Y2Ca)Mg2(SiO4)3 | Iso. m_3_m _(_4/_m_32/m ) : I a_3_d |
9.AD.25 | Uvarovite | Ca3Cr2(SiO4)3 | Iso. m_3_m _(_4/_m_32/m ) : I a_3_d |
9.AD.25 | Eltyubyuite | Ca12Fe3+10Si4O32Cl6 | Iso. 43_m_ : I_43_d |
9.AD.25 | Eringaite | Ca3Sc2(SiO4)3 | Iso. m_3_m _(_4/_m_32/m ) : I a_3_d |
9.AD.25 | Henritermierite | Ca3Mn3+2(SiO4)2[◻(OH)4] | Tet. 4/m m m _(_4/_m_2/_m_2/m ) : _I_41/a c d |
9.AD.25 va | Hydrougrandite | (Ca,Mg,Fe2+)3(Fe3+,Al)2[(OH)4(SiO4)2] | Iso. |
9.AD.25 | Calderite | Mn2+3Fe3+2(SiO4)3 | Iso. m_3_m _(_4/_m_32/m ) : I a_3_d |
9.AD.25 | Nikmelnikovite | Ca12(Fe2+Fe3+3Al3◻)[SiO4]6[◻(OH)4]5◻4 | Trig. 3 : _R_3 |
9.AD.25 | Hutcheonite | Ca3Ti2(SiO4)(AlO4)2 | Iso. m_3_m _(_4/_m_32/m ) : I a_3_d |
9.AD.25 | Wadalite | (Ca,Mg)6(Al,Fe3+)4((Si,Al)O4)3O4Cl3 | Iso. 43_m_ : I_43_d |
9.AD.25 | Rubinite | Ca3Ti3+2Si3O12 | Iso. m_3_m _(_4/_m_32/m ) : I a_3_d |
9.AD.25 | Kerimasite | Ca3Zr2(SiO4)(Fe3+O4)2 | Iso. m_3_m _(_4/_m_32/m ) : I a_3_d |
9.AD.25 | Holtstamite | Ca3Al2(SiO4)2[◻(OH)4] | Tet. 4/m m m _(_4/_m_2/_m_2/m ) : _I_41/a c d |
9.AD.25 | Spessartine | Mn2+3Al2(SiO4)3 | Iso. m_3_m _(_4/_m_32/m ) : I a_3_d |
9.AD.25 | Toturite | Ca3Sn2(SiO4)(Fe3+O4)2 | Iso. m_3_m _(_4/_m_32/m ) : I a_3_d |
9.AD.25 | Kimzeyite | Ca3Zr2(SiO4)(AlO4)2 | Iso. m_3_m _(_4/_m_32/m ) : I a_3_d |
9.AD.25 | Khoharite | Mg3Fe3+2(SiO4)3 | |
9.AD.25 | Irinarassite | Ca3Sn2(SiO4)(AlO4)2 | Iso. m_3_m _(_4/_m_32/m ) : I a_3_d |
9.AD.25 | Knorringite | Mg3Cr2(SiO4)3 | Iso. m_3_m _(_4/_m_32/m ) : I a_3_d |
9.AD.25 | Goldmanite | Ca3V3+2(SiO4)3 | Iso. m_3_m _(_4/_m_32/m ) : I a_3_d |
9.AD.25 | Blythite | Mn2+3Mn3+2[SiO4]3 | |
9.AD.25 | Skiagite | Fe2+3Fe3+2[SiO4]3 | |
9.AD.25 | UM1984-37-SiO:CrMn | Mn2+3Cr3+2(SiO4)3 | |
9.AD.25 | Almandine | Fe2+3Al2(SiO4)3 | Iso. m_3_m _(_4/_m_32/m ) : I a_3_d |
9.AD.25 va | Yamatoite | (Mn2+,Ca)3(V3+,Al)2(SiO4)3 | Iso. |
9.AD.25 | Momoiite | Mn2+3V3+2(SiO4)3 | Iso. m_3_m _(_4/_m_32/m ) : I a_3_d |
9.AD.25 | Grossular | Ca3Al2(SiO4)3 | Iso. m_3_m _(_4/_m_32/m ) : I a_3_d |
9.AD.25 | Andradite | Ca3Fe3+2(SiO4)3 | Iso. m_3_m _(_4/_m_32/m ) : I a_3_d |
9.AD.25 | Morimotoite | Ca3(TiFe2+)(SiO4)3 | Iso. m_3_m _(_4/_m_32/m ) : I a_3_d |
9.AD.25 | Majorite | Mg3(MgSi)(SiO4)3 | Iso. m_3_m _(_4/_m_32/m ) : I a_3_d |
9.AD.25 | Pyrope | Mg3Al2(SiO4)3 | Iso. m_3_m _(_4/_m_32/m ) : I a_3_d |
9.AD.25 | Schorlomite | Ca3Ti2(SiO4)(Fe3+O4)2 | Iso. m_3_m _(_4/_m_32/m ) : I a_3_d |
9.AD.30 | Hafnon | HfSiO4 | Tet. 4/m m m _(_4/_m_2/_m_2/m ) : _I_41/a m d |
9.AD.30 | Zircon | Zr(SiO4) | Tet. 4/m m m _(_4/_m_2/_m_2/m ) : _I_41/a m d |
9.AD.30 | Coffinite | U(SiO4) · nH2O | Tet. 4/m m m _(_4/_m_2/_m_2/m ) : _I_41/a m d |
9.AD.30 | Thorite | Th(SiO4) | Tet. 4/m m m _(_4/_m_2/_m_2/m ) : _I_41/a m d |
9.AD.30 va | Auerlite | near Th(Si,P)O4 | |
9.AD.30 | Stetindite-(Ce) | Ce(SiO4) | Tet. 4/m m m _(_4/_m_2/_m_2/m ) : _I_41/a m d |
9.AD.35 | Tombarthite-(Y) | Y4(Si,H4)4O12-x(OH)4+2x | Mon. |
9.AD.35 | Huttonite | ThSiO4 | Mon. 2/m |
9.AD.40 | Eulytine | Bi4(SiO4)3 | Iso. 43_m_ : I_43_d |
9.AD.45 | Reidite | ZrSiO4 | Tet. 4/m : _I_41/a |
9.AD.55 | Jeffbenite | Mg3Al2Si3O12 | Tet. 42_m_ : I_42_d |
Other InformationHide
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Notes:
Dissolves readily in the weakest acids, leaving a silica pseudomorph, gives no effervescence, and yields abundant evidence of calcium.
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 BredigiteHide
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References for BredigiteHide
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Reference List:
Žáček, Vladimír, Skála, Roman, Chlupáčová, Marta, Dvořák, (2005) Ca-Fe3+-rich, Si-undersaturated buchite from Zelenky, North-Bohemian Brown Coal Basin, Czech Republic. European Journal of Mineralogy, 17 (4). 623-634 doi:10.1127/0935-1221/2005/0017-0623
Kahlenberg, Volker, Galuskina, Irina, Krüger, Biljana, Pauluhn, Anuschka, Galuskin, Evgeny (2019) Structural investigations on bredigite from the Hatrurim Complex. Mineralogy and Petrology, 113 (2) 261-272 doi:10.1007/s00710-018-0646-z
Localities for BredigiteHide
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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.