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Middlebackite
A valid IMA mineral species
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About Middlebackite
Formula:
Cu2C2O4(OH)2
Colour:
Turquoise-blue
Lustre:
Vitreous
Hardness:
2
Specific Gravity:
3.64 (Calculated)
Crystal System:
Monoclinic
Name:
For the Middleback Range, in which the type locality is situated.
Unique Identifiers
Mindat ID:
47562
Long-form identifier:
mindat:1:1:47562:6
IMA Classification of Middlebackite
Approved
IMA Formula:
Cu2+2(C2)6+O4(OH)2
Approval year:
2016
First published:
2019
Classification of Middlebackite
10.AB.50
10 : ORGANIC COMPOUNDS
A : Salts of organic acids
B : Oxalates
10 : ORGANIC COMPOUNDS
A : Salts of organic acids
B : Oxalates
Mineral Symbols
As of 2021 there are now IMA–CNMNC approved mineral symbols (abbreviations) for each mineral species, useful for tables and diagrams.
| Symbol | Source | Reference for Standard |
|---|---|---|
| Mbk | 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 Middlebackite
Vitreous
Transparency:
Translucent
Colour:
Turquoise-blue
Streak:
Pale blue
Hardness:
2 on Mohs scale
Tenacity:
Brittle
Cleavage:
Perfect
Fracture:
Irregular/Uneven
Density:
3.64 g/cm3 (Calculated)
Comment:
Calculated based on empirical formula
Optical Data of Middlebackite
Type:
Biaxial (+)
RI values:
nα = 1.663(4) nβ = 1.748(4) nγ = 1.861(4)
2V:
Calculated: 86.7°
Max. Birefringence:
δ = 0.198
Based on recorded range of RI values above.
Based on recorded range of RI values above.
Interference Colours:
The colours simulate birefringence patterns seen in thin section under crossed polars. They do not take into account mineral colouration or opacity.
Michel-Levy Bar The default colours simulate the birefringence range for a 30 µm thin-section thickness. Adjust the slider to simulate a different thickness.
Grain Simulation You can rotate the grain simulation to show how this range might look as you rotated a sample under crossed polars. Each grain retains its interference colour (retardation) while its brightness falls to black at extinction and reaches a maximum between extinction positions.
The colours simulate birefringence patterns seen in thin section under crossed polars. They do not take into account mineral colouration or opacity.
Michel-Levy Bar The default colours simulate the birefringence range for a 30 µm thin-section thickness. Adjust the slider to simulate a different thickness.
Grain Simulation You can rotate the grain simulation to show how this range might look as you rotated a sample under crossed polars. Each grain retains its interference colour (retardation) while its brightness falls to black at extinction and reaches a maximum between extinction positions.
Surface Relief:
Very High (positive)
Relative to Canada balsam mounting medium (n ≈ 1.537).
Relative to Canada balsam mounting medium (n ≈ 1.537).
This shows the grain boundary and Becke line effect under plane-polarised
light, based on the contrast between this mineral's average refractive
index and the mounting medium. It does not take into account mineral
colouration.
In focus
Interference Figure:
This shows the idealized biaxial acute bisectrix (Bxa) interference figure
- the conoscopic view for a grain cut perpendicular to the acute bisectrix, using
this mineral's 2V. The two small white dots mark the melatopes - the points
where the two optic axes emerge - and are shown only when they fall within the
field of view. The coloured bands are isochromatics, and the dark bands are
isogyres.
Rotate the stage: at 0°/90° the isogyres form a cross through the melatopes; at 45° they pull apart into curved hyperbolas. That splitting on rotation - absent in a uniaxial figure - is the standard diagnostic test for telling biaxial minerals from uniaxial ones. If 2V is large, the melatopes may fall outside the field of view, as they often do at the microscope too.
Rotate the stage: at 0°/90° the isogyres form a cross through the melatopes; at 45° they pull apart into curved hyperbolas. That splitting on rotation - absent in a uniaxial figure - is the standard diagnostic test for telling biaxial minerals from uniaxial ones. If 2V is large, the melatopes may fall outside the field of view, as they often do at the microscope too.
Dispersion:
slight, r>v
Pleochroism:
Visible
Comments:
X = colourless, Y = very pale blue, Z = dark sky blue; Z>Y>X
Chemistry of Middlebackite
Mindat Formula:
Cu2C2O4(OH)2
Element Weights:
Elements listed:
Crystallography of Middlebackite
Crystal System:
Monoclinic
Class (H-M):
2/m - Prismatic
Space Group:
P21/c
Setting:
P21/c
X-Ray Powder Diffraction
Powder Diffraction Data:
| d-spacing | Intensity |
|---|---|
| 7.070 Å | (16) |
| 3.739 Å | (100) |
| 2.860 Å | (18) |
| 2.481 Å | (12) |
| 2.350 Å | (9) |
Geological Environment
Paragenetic Mode(s):
| Paragenetic Mode | Earliest Age (Ga) |
|---|---|
| Stage 10a: Neoproterozoic oxygenation/terrestrial biosphere | <0.6 |
| 53 : Other minerals with taphonomic origins | <0.4 |
Type Occurrence of Middlebackite
General Appearance of Type Material:
Aggregates of blue prismatic crystals up to 0.3 mm across. Individual crystals are up to 0.05 mm long.
Place of Conservation of Type Material:
South Australian Museum, Adelaide, South Australia, Registration number G34300.
Associated Minerals at Type Locality:
Synonyms of Middlebackite
Other Language Names for Middlebackite
Dutch:Middlebackiet
German:Middlebackit
Common Associates
Associations Based on Photo Data:
Related Minerals - Strunz-mindat Grouping
| 10.AB. | Deveroite-(Ce) | Ce2(C2O4)3 · 10H2O |
| 10.AB. | Edwindavisite | Cu(C2O4)(NH3) |
| 10.AB.X | Falottaite | MnC2O4 · 3H2O |
| 10.AB. | Uroxite | [(UO2)2(C2O4)(OH)2(H2O)2] · H2O |
| 10.AB.05 | Katsarosite | Zn(C2O4) · 2H2O |
| 10.AB.05 | Andreybulakhite | Ni(C2O4) · 2H2O |
| 10.AB.05 | Humboldtine | Fe2+(C2O4) · 2H2O |
| 10.AB.05 | Lindbergite | Mn2+(C2O4) · 2H2O |
| 10.AB.10 | Glushinskite | Mg(C2O4) · 2H2O |
| 10.AB.15 | Moolooite | Cu(C2O4) · nH2O |
| 10.AB.20 | Stepanovite | NaMgFe3+(C2O4)3 · 8-9H2O |
| 10.AB.25 | Minguzzite | K3Fe3+(C2O4)3 · 3H2O |
| 10.AB.30 | Wheatleyite | Na2Cu(C2O4)2 · 2H2O |
| 10.AB.35 | Zhemchuzhnikovite | NaMgAl(C2O4)3 · 8H2O |
| 10.AB.40 | Weddellite | Ca(C2O4) · (2.5-x)H2O |
| 10.AB.45 | Whewellite | Ca(C2O4) · H2O |
| 10.AB.47 | Fiemmeite | Cu2(C2O4)(OH)2 · 2H2O |
| 10.AB.50 | Caoxite | Ca(C2O4) · 3H2O |
| 10.AB.52 | Metauroxite | (UO2)2(C2O4)(OH)2(H2O)2 |
| 10.AB.55 | Oxammite | (NH4)2(C2O4) · H2O |
| 10.AB.60 | Natroxalate | Na2(C2O4) |
| 10.AB.60 | Phoxite | (NH4)2Mg2(C2O4)(PO3OH)2(H2O)4 |
| 10.AB.60 | Carboferriphoxite | [(NH4)K(H2CO3)][Fe3+(HPO4)(H2PO4)(C2O4)] |
| 10.AB.60 | Ferriphoxite | [(NH4)2K(H2O)][Fe3+(HPO4)2(C2O4)] |
| 10.AB.65 | Coskrenite-(Ce) | Ce2(SO4)2(C2O4) · 8H2O |
| 10.AB.70 | Levinsonite-(Y) | (Y,Nd,La)Al(C2O4)(SO4)2 · 12H2O |
| 10.AB.75 | Zugshunstite-(Ce) | (Ce,Nd,La)Al(C2O4)(SO4)2 · 12H2O |
| 10.AB.80 | Novgorodovaite | Ca2(C2O4)Cl2 · 2H2O |
Other Information
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 Middlebackite
mindat.org URL:
https://www.mindat.org/min-47562.html
Please feel free to link to this page.
Please feel free to link to this page.
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External Links:
Mineral Dealers:
References for Middlebackite
Reference List:
Hålenius, U., Hatert, F., Pasero, M., Mills, S.J. (2016) New minerals and nomenclature modifications approved in 2016, CNMNC Newsletter no 30. Mineralogical Magazine, 80 (2) 407-413 doi:10.1180/minmag.2016.080.081
Demartin, Francesco, Campostrini, Italo, Ferretti, Paolo, Rocchetti, Ivano (2017) Secondo ritrovamento mondiale di middlebackite presso il Passo di San Lugano (Carano, Trento, Italia) [Second global occurrence of middlebackite near the Passo di San Lugano (Carano, Trento, Italy) ]. Geo.Alp, 14. Bolzano/Bozen. 35-38
Localities for Middlebackite
Showing 7 localities.
Locality List
- 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).
All localities listed without proper references should be considered as questionable.
Australia (TL) | |
| Pring et al. (2000) +1 other reference |
| mineral middlebackite [Cu2C2O4 (OH) +4 other references |
| O’Connor et al. (2019) | |
Italy | |
| Ferretti et al. (2017) |
| Demartin et al. (2017) +3 other references |
| Domenico Saccardo et al. (2019) +1 other reference |
| Rocchetti (2019: Aggiornamento 2019 sulla mineralogia vicentina. Moolooite e middlebackite di Valle Cumerlati.Studi e Ricerche - Associazione Amici del Museo - Museo Civico “G. Zannato”, 26, 46-47) |
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symbol to view information about a locality.
The
Val Gardena Sandstone exposure, San Lugano pass, Carano, Ville di Fiemme, Trento Province, Trentino-Alto Adige/Südtirol, Italy