登录注册
搜索:
矿物名称:
地区产地名称:
关键字:
 
主页关于 MindatMindat手册Mindat的历史版权我们是谁我们的科学研究Mindat 通讯 [免费下载]联系我们
捐赠给 Mindat赞助板页企业赞助已赞助的板页
学习中心什么是矿物?地球上最常见的矿物教育工作者信息Mindat 文章Mindat 通讯 [免费下载]元素矿物测验
Search Form搜索矿物的性质搜索矿物的化学矿物可视化浏览器高级地点搜索随意显示任何一 种矿物随机地点使用minID搜索按国家查找矿物矿物字母索引产地字母索引矿物共生组合搜索国家列表邻近产地照片搜索搜索文章搜索词汇表Rock H. Currier数字图书馆更多搜索选项
Mindat手册添加新照片评价照片产区编辑报告坐标完成报告添加词汇表项目
矿物岩石学化石陨石地质时代
矿业公司统计矿物博物馆矿物学会与组织矿物展及活动设备设置时光机
阅读讨论鉴定请求
照片搜索图片画廊按颜色搜索照片颜色浏览器今天最新的照片昨天最新的照片用户照片相集过去每日精选照片相集摄影

Schindlerite

A valid IMA mineral species
This page is currently not sponsored. Click here to sponsor this page.
Hide all sections | Show all sections

About SchindleriteHide

09185090017917324265341.jpg
Dr, Michael Schindler
Formula:
{(NH4)4Na2(H2O)10}{V10O28}
Colour:
Orange
Lustre:
Sub-Adamantine
Hardness:
2
Specific Gravity:
2.461 (Calculated)
Crystal System:
Triclinic
Name:
Named in honor of Dr. Michael Schindler (b. 1966, Frankfurt, Germany), professor at University of Manitoba, Canada. He has worked extensively on the structures of vanadium minerals.

Unique IdentifiersHide

Mindat ID:
43584
Long-form identifier:
mindat:1:1:43584:0

Classification of SchindleriteHide

00669880017683444897551.jpg
The Decavanadate Cluster

The decavanadate cluster found in schindlerite. The same cluster is known in a number of other secondary vanadium minerals including, for example, pascoite, magnesiopascoite, and huemulite.

IMA Classification of SchindleriteHide

Approved
IMA status notes:
Redefined by the IMA
IMA Formula:
(N3-H4)4Na2[V5+10O28]·10H2O
Approval year:
2012
First published:
2013
Approval history:
Originally approved as a hydronium mineral (IMA 2012–063), later redefined as an ammonium-bearing decavanadate mineral (Proposal IMA 15-G).
4.HC.60

4 : OXIDES (Hydroxides, V[5,6] vanadates, arsenites, antimonites, bismuthites, sulfites, selenites, tellurites, iodates)
H : V[5,6] Vanadates
C : [6]-Sorovanadates

Mineral SymbolsHide

As of 2021 there are now IMA–CNMNC approved mineral symbols (abbreviations) for each mineral species, useful for tables and diagrams.

SymbolSourceReference for Standard
ShiIMA–CNMNCWarr, L.N. (2021). IMA–CNMNC approved mineral symbols. Mineralogical Magazine, 85(3), 291-320. doi:10.1180/mgm.2021.43

Physical Properties of SchindleriteHide

Sub-Adamantine
Transparency:
Transparent
Colour:
Orange
Streak:
Yellow
Hardness:
Tenacity:
Brittle
Cleavage:
Perfect
{010}
Density:
2.461 g/cm3 (Calculated)

Optical Data of SchindleriteHide

Type:
Biaxial (+)
RI values:
nα = 1.74 nβ = 1.790(5) nγ = 1.875
2V:
Measured: 78° (1)
Max. Birefringence:
δ = 0.135
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.

Surface Relief:
Very High (positive)
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.
Dispersion:
r > v, very strong
Optical Extinction:
X ∧ b = 25°; Y ∧ c = 12°; Z ∧ a = 3°.
Pleochroism:
Not Visible
Comments:
α- estimated, γ - calculated
Minerals reacted with RI fluids

Chemistry of SchindleriteHide

Mindat Formula:
{(NH4)4Na2(H2O)10}{V10O28}
Element Weights:
Element% weight
O48.418 %
V40.569 %
N4.462 %
Na3.662 %
H2.890 %

Calculated from ideal end-member formula.
O
V
N
Na
H

Crystallography of SchindleriteHide

Crystal System:
Triclinic
Class (H-M):
1 - Pinacoidal
Space Group:
P1
Cell Parameters:
a = 8.5143(3) Å, b = 10.4283(5) Å, c = 11.2827(8) Å
α = 68.595(5)°, β = 87.253(6)°, γ = 67.112(5)°
Ratio:
a:b:c = 0.816 : 1 : 1.082
Unit Cell V:
854.08 ų (Calculated from Unit Cell)
Z:
1
Morphology:
Tabular on {011} and often occur in stacked parallel intergrowths. Forms observed include {100}, {010}, {001}, {110}, {011}, {111}, and {111}.

Crystal StructureHide

Load
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
Display Options
Black Background | White Background
Perspective On | Perspective Off
2D | Stereo | Red-Blue | Red-Cyan
View
CIF File    Best | x | y | z | a | b | c
Rotation
Stop | Start
Labels
Console Off | On | Grey | Yellow
IDSpeciesReferenceLinkYearLocalityPressure (GPa)Temp (K)
0019899SchindleriteKampf A R, Hughes J M, Marty J, Nash B (2013) Wernerbaurite, {[Ca(H2O)7]2(H2O)2(H3O)2}{V10O28}, and schindlerite, {[Na2(H2O)10](H3O)4}{V10O28}, the first hydronium-bearing decavanadate minerals The Canadian Mineralogist 51 297-3122013St. Jude mine, San Miguel County, Colorado, U.S.A.0293
CIF Raw Data - click here to close

X-Ray Powder DiffractionHide

Geological EnvironmentHide

Paragenetic Mode(s):
Paragenetic ModeEarliest Age (Ga)
Stage 7: Great Oxidation Event<2.4
47a : [Near-surface hydration of prior minerals]
47e : [Vanadates, chromates, manganates]
Stage 10a: Neoproterozoic oxygenation/terrestrial biosphere<0.6
53 : Other minerals with taphonomic origins<0.4
Stage 10b: Anthropogenic minerals<10 Ka
55 : Anthropogenic mine minerals

Type Occurrence of SchindleriteHide

General Appearance of Type Material:
Tabular on {011} and often occur in stacked parallel intergrowths. Individual crystals are up to 0.3 mm in maximum dimension.
Place of Conservation of Type Material:
Natural History Museum of Los Angeles County, Los Angeles, California, USA, catalogue numbers 64005, 64006 and 64007.
Geological Setting of Type Material:
Oxidation of montroseite-corvusite assemblages in a moist environment.
Associated Minerals at Type Locality:

Synonyms of SchindleriteHide

Other Language Names for SchindleriteHide

Relationship of Schindlerite to other SpeciesHide

Other Members of Pascoite Family:
Ammoniolasalite[(NH4)2Mg2(H2O)20] [V10O28]Mon. 2/m : B2/b
BluestreakiteK4Mg2(V4+2V5+8O28) · 14H2OMon. 2/m : P21/c
BurroiteCa2(NH4)2(V10O28) · 15H2OTric. 1 : P1
Caseyite[(V5+O2)Al10-x(OH)20-2x(H2O)18-2x]2[H2V4+V5+9O28][V5+10O28]2(Na,K,Ca)2-y(SO4)2-z · (60+8x+y+4z)H2O (x = 0-2.5; y = 0-2; z = 0-2)Mon. 2/m : P21/c
Flatimerite[Al13(OH)24(H2O)24][V5+9V4+O28] · [(SO4)4(H2O)24]Tric. 1 : P1
GunteriteNa4Ca(V10O28) · 20H2OMon. 2/m : B2/m
HuemuliteNa4Mg(V10O28) · 24H2OTric.
HughesiteNa3Al(V10O28) · 22H2OTric. 1 : P1
HummeriteK2Mg2(V10O28) · 16H2OTric. 1 : P1
HydropascoiteCa3(V10O28) · 24H2OTric. 1 : P1
KokinositeNa2Ca2(V10O28) · 24H2OTric. 1 : P1
LasaliteNa2Mg2(V10O28) · 20H2OMon. 2/m : B2/b
MagnesiopascoiteCa2Mg(V10O28) · 16H2OMon. 2/m : B2/m
NashiteNa3Ca2[(V5+9V4+)O28] · 24H2OMon. 2/m : P21/m
OkieiteMg3[V10O28] · 28H2OTric. 1 : P1
PascoiteCa2Ca(V10O28) · 17H2OMon. 2 : B2
PostiteMg(H2O)6Al2(OH)2(H2O)8(V10O28) · 13H2OOrth. mmm(2/m2/m2/m) : Pccn
Protocaseyite[Al4(OH)6(H2O)12][V10O28] · 8H2OTric. 1 : P1
Rakovanite(NH4)3Na3(V10O28) · 12H2OMon. 2/m : P21/c
TrebiskyiteNa3Mg2[TiV9O28] · 22H2OMon. 2/m : P21/c
Wernerbaurite{(NH4)2[Ca2(H2O)14](H2O)2}{V10O28}Tric. 1 : P1

Common AssociatesHide

Associations Based on Photo Data:
3 photos of Schindlerite associated with Corvusite(Na,K,Ca,Mg)2(V5+,V4+,Fe2+)8O20 · 6-10H2O
3 photos of Schindlerite associated with Montroseite(V3+,Fe3+)O(OH)
2 photos of Schindlerite associated with Wernerbaurite{(NH4)2[Ca2(H2O)14](H2O)2}{V10O28}
2 photos of Schindlerite associated with BurroiteCa2(NH4)2(V10O28) · 15H2O
1 photo of Schindlerite associated with GypsumCaSO4 · 2H2O
1 photo of Schindlerite associated with 'Petrified Wood'
1 photo of Schindlerite associated with 'Sandstone'

Related Minerals - Strunz-mindat GroupingHide

4.HC.Protocaseyite[Al4(OH)6(H2O)12][V10O28] · 8H2OTric. 1 : P1
4.HC.Ammoniolasalite[(NH4)2Mg2(H2O)20] [V10O28]Mon. 2/m : B2/b
4.HC.BeckettiteCa2V6Al6O20Tric. 1 : P1
4.HC.Flatimerite[Al13(OH)24(H2O)24][V5+9V4+O28] · [(SO4)4(H2O)24]Tric. 1 : P1
4.HC.05PascoiteCa2Ca(V10O28) · 17H2OMon. 2 : B2
4.HC.05HydropascoiteCa3(V10O28) · 24H2OTric. 1 : P1
4.HC.05LasaliteNa2Mg2(V10O28) · 20H2OMon. 2/m : B2/b
4.HC.05HughesiteNa3Al(V10O28) · 22H2OTric. 1 : P1
4.HC.05MagnesiopascoiteCa2Mg(V10O28) · 16H2OMon. 2/m : B2/m
4.HC.05Rakovanite(NH4)3Na3(V10O28) · 12H2OMon. 2/m : P21/c
4.HC.10HummeriteK2Mg2(V10O28) · 16H2OTric. 1 : P1
4.HC.15SherwooditeCa5.5(AlV4+V5+12O39) · 28H2OTet. 4/mmm(4/m2/m2/m) : I41/amd
4.HC.20BluestreakiteK4Mg2(V4+2V5+8O28) · 14H2OMon. 2/m : P21/c
4.HC.25Wernerbaurite{(NH4)2[Ca2(H2O)14](H2O)2}{V10O28}Tric. 1 : P1
4.HC.25BurroiteCa2(NH4)2(V10O28) · 15H2OTric. 1 : P1
4.HC.30Caseyite[(V5+O2)Al10-x(OH)20-2x(H2O)18-2x]2[H2V4+V5+9O28][V5+10O28]2(Na,K,Ca)2-y(SO4)2-z · (60+8x+y+4z)H2O (x = 0-2.5; y = 0-2; z = 0-2)Mon. 2/m : P21/c
4.HC.35GunteriteNa4Ca(V10O28) · 20H2OMon. 2/m : B2/m
4.HC.40KokinositeNa2Ca2(V10O28) · 24H2OTric. 1 : P1
4.HC.45NashiteNa3Ca2[(V5+9V4+)O28] · 24H2OMon. 2/m : P21/m
4.HC.50OkieiteMg3[V10O28] · 28H2OTric. 1 : P1
4.HC.55PostiteMg(H2O)6Al2(OH)2(H2O)8(V10O28) · 13H2OOrth. mmm(2/m2/m2/m) : Pccn

Other InformationHide

IR Spectrum:
none
Notes:
Dissolves instantly in cold, dilute HCl and slowly in water
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 SchindleriteHide

References for SchindleriteHide

Localities for SchindleriteHide

Showing 3 localities.

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.
Hide all sections | Show all sections

Locality ListHide

- 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
 
  • Colorado
    • Mesa County
      • Gateway Mining District
        • Beaver Mesa
Tony Kampf Identification
    • San Miguel County
Kampf et al. (2019)
    • Slick Rock Mining District
Kampf et al. (2013)
 
and/or  
版权所有© mindat.org1993年至2026年,除了规定的地方。 Mindat.org全赖于全球数千个以上成员和支持者们的参与。
Content on this site may not be used to train, fine-tune, or otherwise develop artificial intelligence or machine learning models without prior written permission - see our Terms & Conditions.
To cite: Ralph, J., Von Bargen, D., Martynov, P., Zhang, J., Que, X., Prabhu, A., Morrison, S. M., Li, W., Chen, W., & Ma, X. (2025). Mindat.org: The open access mineralogy database to accelerate data-intensive geoscience research. American Mineralogist, 110(6), 833–844. doi:10.2138/am-2024-9486.
隐私政策 - 条款和条款细则 - 联络我们 - Report a bug/vulnerability 当前服务器日期和时间: 2026.11.1 13:41:25 页面生成: 2026.10.11 15:29:35
Go to top of page