Stanevansite (original) (raw)

A valid IMA mineral species

Formula:

Mg(C2H3O3)2 · 2H2O

Crystal System:

Monoclinic

The second glycolate mineral to date. Associated with the first one - lazaraskeite. The third glycolate mineral is jimkrieghite; and the fourth - lianbinite (NH4; more complex).

The structure is based on mononuclear complexes, [Mg(C2H3O3)2(H2O)2], connected to one another by hydrogen bonds.

Unique IdentifiersHide

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Long-form identifier:

mindat:1:1:470464:1

63b9d49f-33d4-424d-9816-c609735dd41c

IMA Classification of StanevansiteHide

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Approval history:

IMA 2022-085

Classification of StanevansiteHide

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10.AA.

10 : ORGANIC COMPOUNDS
A : Salts of organic acids
A : Formates, Acetates, etc.

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
Ses 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 StanevansiteHide

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Density:

1.69(2) g/cm3 (Measured) 1.682 g/cm3 (Calculated)

Optical Data of StanevansiteHide

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RI values:

_n_α = 1.539(5) _n_β = 1.545(5) _n_γ = 1.558(5)

2V:

Measured: 62° (2), Calculated: 69°

δ = 0.019

Image shows birefringence interference colour range (at 30µm thickness)
and does not take into account mineral colouration.

Chemistry of StanevansiteHide

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Mindat Formula:

Mg(C2H3O3)2 · 2H2O

Chemical AnalysisHide

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Empirical formulas:

Sample ID Empirical Formula
1 (Mg0.95Zn0.05)Σ1.00(C2H3O3)2.2H2O

Sample references:

ID Locality Reference Notes
1 Western end, Pusch Ridge, Pima County, Arizona, USA Yang, H., Gu, X., Lazar, W., Gibbs, R.B., Downs, R.T. (2024): Stanevansite, Mg(C2H3O3)2·2H2O, a New Hydrous Glycolate Mineral, From The Santa Catalina Mountains, Tucson, Arizona, USA. The Canadian Journal of Mineralogy and Petrology, 62, (in press).

Crystallography of StanevansiteHide

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Crystal System:

Monoclinic

Class (H-M):

2/m - Prismatic

Cell Parameters:

a = 11.4927(2) Å, b = 5.8547(1) Å, c = 12.4711(2) Å
β = 91.161(1)°

Ratio:

a:b:c = 1.963 : 1 : 2.13

Unit Cell V:

838.96 ų (Calculated from Unit Cell)

Twinning:

common on (100).

X-Ray Powder DiffractionHide

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Powder Diffraction Data:

d-spacing Intensity
5.47 Å (62)
5.223 Å (93)
4.787 Å (100)
3.819 Å (73)
3.102 Å (71)
3.018 Å (33)
2.580 Å (20)
2.406 Å (33)

Type Occurrence of StanevansiteHide

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General Appearance of Type Material:

occurs as sprays of bladed crystals (up to 0.40 × 0.07 × 0.03 mm).

Place of Conservation of Type Material:

Type material is deposited in the collections of the University of Arizona Alfie Norville Gem & Mineral Museum, 115 N Church Ave Ste 121, Tucson, AZ 85701, USA, catalogue number 22721 (holotype), and the RRUFF Project, deposition number R220011 (cotype)

Associated Minerals at Type Locality:

Synonyms of StanevansiteHide

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Relationship of Stanevansite to other SpeciesHide

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Other Members of this group:

Common AssociatesHide

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Associated Minerals Based on Photo Data:

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Other InformationHide

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Notes:

It is insoluble in water, but slowly dissolves in hydrochloric acid.

Health Risks:

No information on health risks for this material has been entered into the database. You should always treat mineral specimens with care.

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References for StanevansiteHide

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Reference List:

Yang, Hexiong, Gu, Xiangping, Lazar, Warren, Gibbs, Ronald B., Downs, Robert T. (2024) Stanevansite, Mg(C2H3O3)2·2H2O, a New Hydrous Glycolate Mineral, From The Santa Catalina Mountains, Tucson, Arizona, USA. The Canadian Journal of Mineralogy and Petrology, 62 (1) 153-164 doi:10.3749/2300047

Localities for StanevansiteHide

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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.

USA (TL)
Arizona Pima County Pusch Ridge Western end (TL) Miyawaki et al. (2022)