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Gravegliaite
A valid IMA mineral species
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About Gravegliaite
Unique Identifiers
Mindat ID:
1742
Long-form identifier:
mindat:1:1:1742:4
IMA Classification of Gravegliaite
Approved
IMA Formula:
Mn2+S4+O3·3H2O
Approval year:
1990
First published:
1991
Classification of Gravegliaite
4.JE.05
4 : OXIDES (Hydroxides, V[5,6] vanadates, arsenites, antimonites, bismuthites, sulfites, selenites, tellurites, iodates)
J : Arsenites, antimonites, bismuthites, sulfites, selenites, tellurites; iodates
E : Sulfites
4 : OXIDES (Hydroxides, V[5,6] vanadates, arsenites, antimonites, bismuthites, sulfites, selenites, tellurites, iodates)
J : Arsenites, antimonites, bismuthites, sulfites, selenites, tellurites; iodates
E : Sulfites
Dana 7th ed.:
34.2.4.2
34.2.5.2
34 : SELENITES, TELLURITES AND SULFITES
2 : A(XO3)·xH2O
34 : SELENITES, TELLURITES AND SULFITES
2 : A(XO3)·xH2O
27.1.3
27 : Sulphites, Chromates, Molybdates and Tungstates
1 : Sulphites
27 : Sulphites, Chromates, Molybdates and Tungstates
1 : Sulphites
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 |
|---|---|---|
| Gvg | 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 Gravegliaite
Vitreous
Transparency:
Transparent
Colour:
Colorless
Streak:
White
Cleavage:
Distinct/Good
Parallel to [010].
Parallel to [010].
Fracture:
None observed
Density:
2.39 g/cm3 (Calculated)
Optical Data of Gravegliaite
Type:
Biaxial (+)
RI values:
nα = 1.590(2) nβ = 1.596(2) nγ = 1.636(2)
2V:
Measured: 41° (3), Calculated: 43°
Max. Birefringence:
δ = 0.046
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:
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:
r > v distinct
Optical Extinction:
Z = b.
Pleochroism:
Non-pleochroic
Chemistry of Gravegliaite
Mindat Formula:
Mn2+SO3 · 3H2O
Element Weights:
Elements listed:
Crystallography of Gravegliaite
Crystal System:
Orthorhombic
Class (H-M):
mmm(2/m2/m2/m) - Dipyramidal
Space Group:
Pnma
Setting:
Pnma
Cell Parameters:
a = 9.763(1) Å, b = 5.635(1) Å, c = 9.558(1) Å
Ratio:
a:b:c = 1.733 : 1 : 1.696
Unit Cell V:
525.83 ų (Calculated from Unit Cell)
Z:
4
Crystal Structure
Load
Unit Cell | Unit Cell Packed
2x2x2 | 3x3x3 | 4x4x4
Unit Cell | Unit Cell Packed
2x2x2 | 3x3x3 | 4x4x4
Show
Big Balls | Small Balls | Just Balls | Spacefill
Polyhedra Off | Si Polyhedra | All Polyhedra
Remove metal-metal sticks
Big Balls | Small Balls | Just Balls | Spacefill
Polyhedra Off | Si Polyhedra | All Polyhedra
Remove metal-metal sticks
Display Options
Black Background | White Background
Perspective On | Perspective Off
2D | Stereo | Red-Blue | Red-Cyan
Black Background | White Background
Perspective On | Perspective Off
2D | Stereo | Red-Blue | Red-Cyan
View
CIF File Best | x | y | z | a | b | c
CIF File Best | x | y | z | a | b | c
Rotation
Stop | Start
Stop | Start
Labels
Console Off | On | Grey | Yellow
Console Off | On | Grey | Yellow
Data courtesy of the American Mineralogist Crystal Structure Database. Click on an AMCSD ID to view structure
| ID | Species | Reference | Link | Year | Locality | Pressure (GPa) | Temp (K) |
|---|---|---|---|---|---|---|---|
| 0011006 | Gravegliaite | Basso R, Lucchetti G, Palenzona A (1991) Gravegliaite, MnSO3*3H2O, a new mineral from Val Graveglia (Northern Apennines, Italy) Zeitschrift fur Kristallographie 197 97-106 | ![]() | 1991 | Gambatesa mine, Val Graveglia, Northern Apennines, Italy | 0 | 293 |
CIF Raw Data - click here to close
X-Ray Powder Diffraction
Powder Diffraction Data:
| d-spacing | Intensity |
|---|---|
| 4.33 Å | (Very strong) |
| 3.43 Å | (Very strong) |
| 6.83 Å | (Strong) |
| 2.704 Å | (Medium) |
| 2.666 Å | (Medium) |
| 2.414 Å | (Medium) |
| 1.726 Å | (Medium) |
Geological Environment
Paragenetic Mode(s):
| Paragenetic Mode | Earliest Age (Ga) |
|---|---|
| High-? alteration and/or metamorphism | |
| 32 : Ba/Mn/Pb/Zn deposits, including metamorphic deposits | |
| Stage 7: Great Oxidation Event | <2.4 |
| 47a : [Near-surface hydration of prior minerals] | |
| 47b : [Sulfates and sulfites] | |
| 47e : [Vanadates, chromates, manganates] |
Type Occurrence of Gravegliaite
General Appearance of Type Material:
Radial aggregates of prismatic crystals, elongated parallel to [010] and up to 0.5 mm long.
Place of Conservation of Type Material:
Department of Earth Sciences, University of Genoa, Genoa, Ital
Geological Setting of Type Material:
Ophiolite sequence.
Associated Minerals at Type Locality:
Synonyms of Gravegliaite
Other Language Names for Gravegliaite
Related Minerals - Strunz-mindat Grouping
| 4.JE.X | Albertiniite | Fe2+(SO3) · 3H2O |
| 4.JE. | Mikenewite | Mn2+(S4+O3) · 3H2O |
| 4.JE. | Vanpeltite | (Mo2O5)(S4+O3) · 4H2O |
| 4.JE.05 | Fleisstalite | FeSO3 · 3H2O |
| 4.JE.10 | Hannebachite | CaSO3 · H2O |
| 4.JE.15 | Orschallite | Ca3(SO3)2(SO4) · 12H2O |
| 4.JE.20 | Scotlandite | PbSO3 |
| 4.JE.25 | Kollerite | (NH4)2Fe3+(SO3)2(OH) · H2O |
Other Information
Notes:
Insoluble in water and in ethyl alcohol, soluble in strong 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 Gravegliaite
mindat.org URL:
https://www.mindat.org/min-1742.html
Please feel free to link to this page.
Please feel free to link to this page.
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References for Gravegliaite
Localities for Gravegliaite
Showing 5 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.
Italy (TL) | |
| 415 (354) +3 other references |
Luxembourg | |
| www.mnhn.lu (n.d.) +1 other reference |
Spain | |
| Dill et al. (2023) |
| Dill et al. (2023) | |
Tanzania | |
| Färber (n.d.) |
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The
Gambatesa Mine, Reppia, Ne, Genoa, Liguria, Italy