Clino-ferri-holmquistite
A valid IMA mineral species
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Formula:
◻Li2(Mg3Fe3+2)(Si8O22)(OH)2
The clino-holmquistite group minerals are monoclinic lithium amphiboles defined with:
A(Na+K+2Ca)< 0.5 apfu,
CLi < 0,5 apfu
Clino-ferri-holmquistite is defined with
C2+ position: Mg dominant
C3+ position: Fe dominant
W position: (OH) dominant
A(Na+K+2Ca)< 0.5 apfu,
CLi < 0,5 apfu
Clino-ferri-holmquistite is defined with
C2+ position: Mg dominant
C3+ position: Fe dominant
W position: (OH) dominant
Colour:
Black
Lustre:
Vitreous
Hardness:
6
Specific Gravity:
3.19
Crystal System:
Monoclinic
Member of:
Name:
The original material used to describe clino-ferri-holmquistite (IMA1995-045) by Caballero et al (1998) (originally named by them as "ferri-clinoholmquistite") was renamed "sodic-ferri-clinoholmquistite" and finally became Clino-ferro-ferri-holmquistite, its current valid name.
The mineral now named clino-ferri-holmquistite was originally published as ferri-ottoliniite (IMA2001-067) in 2001. In the 2012 amphibole nomenclature, its composition was considered intermediate between clino-ferri-holmquistite and magnesio-riebeckite, and the ottoliniite root name is discredited.
The clino-ferri-holmquistite holotype material empirical formula is A(K0.07Na0.38)B(Na0.70Li1.24Ca0.06)C(Mg1.35Fe2+0.92Mn2+0.13 Zn0.31Fe3+1.71Al0.10Ti0.06Li0.42) Si8 O22 (OH1.51F0.47). As Li>Na in the B position the mineral is considered a clino-ferri-holmquistite, which was approved in september 2014 (Proposal 14-G ).
The mineral now named clino-ferri-holmquistite was originally published as ferri-ottoliniite (IMA2001-067) in 2001. In the 2012 amphibole nomenclature, its composition was considered intermediate between clino-ferri-holmquistite and magnesio-riebeckite, and the ottoliniite root name is discredited.
The clino-ferri-holmquistite holotype material empirical formula is A(K0.07Na0.38)B(Na0.70Li1.24Ca0.06)C(Mg1.35Fe2+0.92Mn2+0.13 Zn0.31Fe3+1.71Al0.10Ti0.06Li0.42) Si8 O22 (OH1.51F0.47). As Li>Na in the B position the mineral is considered a clino-ferri-holmquistite, which was approved in september 2014 (Proposal 14-G ).
This page provides mineralogical data about Clino-ferri-holmquistite.
Unique Identifiers
Mindat ID:
6928
Long-form identifier:
mindat:1:1:6928:7
Similar Names
| Clinoferroholmquistit | A synonym of Clino-holmquistite Root Name Group | |
| Clinoferroholmquistite | ◻Li2[Fe32+Al2]Si8O22(OH,F)2 |
IMA Classification of Clino-ferri-holmquistite
Classification of Clino-ferri-holmquistite
9.00.
9 : SILICATES (Germanates)
0 :
0 :
9 : SILICATES (Germanates)
0 :
0 :
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 |
|---|---|---|
| Cfhlm | 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 Clino-ferri-holmquistite
Vitreous
Transparency:
Translucent
Colour:
Black
Streak:
Grey
Hardness:
6 on Mohs scale
Tenacity:
Brittle
Cleavage:
Perfect
{110}
{110}
Parting:
a (001) parting
Fracture:
Splintery
Density:
3.19 g/cm3 (Measured) 3.25 g/cm3 (Calculated)
Optical Data of Clino-ferri-holmquistite
Type:
Biaxial (+)
RI values:
nα = 1.699(2) nβ = 1.703(2) nγ = 1.708(2)
2V:
Measured: 72° (7), Calculated: 83°
Max. Birefringence:
δ = 0.009
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:
relatively strong
Pleochroism:
Strong
Comments:
X = yellow green, Y = indigo blue and Z = green blue
Comments:
shows anomalous indigo and brown interference colors.
Chemistry of Clino-ferri-holmquistite
Mindat Formula:
◻Li2(Mg3Fe3+2)(Si8O22)(OH)2
The clino-holmquistite group minerals are monoclinic lithium amphiboles defined with:
A(Na+K+2Ca)< 0.5 apfu,
CLi < 0,5 apfu
Clino-ferri-holmquistite is defined with
C2+ position: Mg dominant
C3+ position: Fe dominant
W position: (OH) dominant
The clino-holmquistite group minerals are monoclinic lithium amphiboles defined with:
A(Na+K+2Ca)< 0.5 apfu,
CLi < 0,5 apfu
Clino-ferri-holmquistite is defined with
C2+ position: Mg dominant
C3+ position: Fe dominant
W position: (OH) dominant
Element Weights:
Crystallography of Clino-ferri-holmquistite
Crystal System:
Monoclinic
Class (H-M):
2/m - Prismatic
Space Group:
B2/m
Setting:
C2/m
Cell Parameters:
a = 9.48 Å, b = 17.845 Å, c = 5.283 Å
β = 102.03°
β = 102.03°
Ratio:
a:b:c = 0.531 : 1 : 0.296
Unit Cell V:
874.10 ų (Calculated from Unit Cell)
Z:
2
Crystal Structure
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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) |
|---|---|---|---|---|---|---|---|
| 0020050 | Clino-ferri-holmquistite | Oberti R, Camara F, Caballero J M (2004) Ferri-ottoliniite and ferriwhittakerite, two new end-members of the new Group 5 for monoclinic amphiboles American Mineralogist 89 888-893 | ![]() | 2004 | Pedriza massif, Sierra de Guadarrama, Spain | 0 | 293 |
CIF Raw Data - click here to close
Geological Environment
Paragenetic Mode(s):
| Paragenetic Mode | Earliest Age (Ga) |
|---|---|
| Near-surface Processes | |
| 22 : Hydration and low-? subsurface aqueous alteration (see also #23) | |
| Stage 4b: Highly evolved igneous rocks | >3.0 |
| 34 : Complex granite pegmatites |
Synonyms of Clino-ferri-holmquistite
Other Language Names for Clino-ferri-holmquistite
Dutch:Clino-ferri-holmquistiet
German:Klino-Ferri-Holmquistit
Japanese:第二鉄単斜ホルムクヴィスト閃石
Russian:Ферриклинохолмквистит
Relationship of Clino-ferri-holmquistite to other Species
Member of:
Other Members of Clino-holmquistite Root Name Group:
| Clino-ferro-ferri-holmquistite | ◻Li2(Fe2+3Fe3+2)(Si8O22)(OH)2 | Mon. 2/m : B2/m |
Related Minerals - Strunz-mindat Grouping
| 9.00. | Mendigite | Mn2Mn2MnCa(Si3O9)2 |
| 9.00. | Alflarsenite | NaCa2Be3Si4O13(OH) · 2H2O |
| 9.00. | Bridgmanite Subgroup | ABSiO3 |
| 9.00. | Ferroericssonite | BaFe2+2 Fe3+(Si2O7)O(OH) |
| 9.00. | Zvyaginite | NaZnNb2Ti[Si2O7]2(OH,F)3(H2O)4+x (x < 1) |
| 9.00. | Burnettite | CaVAlSiO6 |
| 9.00. | Ferrisepiolite | (Fe3+,Fe2+,Mg)4((Si,Fe3+)6O15)(O,OH)2 · 6H2O |
| 9.00. | Yegorovite | Na4[Si4O8(OH)4] · 7H2O |
| 9.00. | Chrysotile | Mg3(Si2O5)(OH)4 |
| 9.00. | 'Shkatulkalita' | |
| 9.00.15 va | 'Chromoamesite' | Mg2(Al,Cr)(AlSiO5)(OH)4 |
| 9.00.50 | Thornasite | Na12Th4+3(Si8O19)4 · 18H2O |
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 Clino-ferri-holmquistite
mindat.org URL:
https://www.mindat.org/min-6928.html
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Please feel free to link to this page.
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References for Clino-ferri-holmquistite
Reference List:
Caballero, Jose M., Monge, Angeles, La Iglesia, Angel, Tornos, Fernando (1998) Ferri-clinoholmquistite, Li2(Fe2+,Mg)3Fe3+2Si8O22(OH)2, a new BLi clinoamphibole from the Pedriza Massif, Sierra de Guadarrama, Spanish Central System. American Mineralogist, 83 (1) 167-171 doi:10.2138/am-1998-1-217
Oberti, Roberta, Cámara, Fernando, Caballero, José Maria (2004) Ferri-ottoliniite and ferriwhittakerite, two new end-members of the new Group 5 for monoclinic amphiboles. American Mineralogist, 89 (5) 888-893 doi:10.2138/am-2004-5-624
Iezzi, G., Cámara, F., Oberti, R., Ventura, G. Della, Pedrazzi, G., Robert, J.-L. (2004) Synthesis, crystal structure and crystal chemistry of ferri-clinoholmquistite, □Li2Mg3Fe3+2Si8O22(OH)2. Physics and Chemistry of Minerals, 31 (6) doi:10.1007/s00269-004-0402-2
Localities for Clino-ferri-holmquistite
Showing 1 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.
Spain | |
| Oberti et al. (2004) |
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