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Khurayyimite

A valid IMA mineral species
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About KhurayyimiteHide

Formula:
Ca7Zn4(Si2O7)2(OH)10 · 4H2O
Colour:
Colorless
Lustre:
Vitreous
Crystal System:
Monoclinic
Name:
Named after the type locality, Khurayyim Mount (Jabal al Khurayyim), Siwaqa pyrometamorphic rock area, Um Al-Rasas Sub-district, central Jordan.
New structure type.

Structure details:
* SiO4 and ZnO2(OH)2 tetrahedra forming (unusual) chains (loop-branched sechser single type, {lB, 11∞}[6Zn4Si4O21]) with Si–Si-Zn sequence;
* neighbouring silicate tetrahedra of the corrugated chains are bridged by additional ZnO2(OH)2 tetrahedra -→ 3-connected dreier rings;
* the chains are merged via clusters of five CaO6 and two CaO7 polyhedra.

The mineral is reported to "belong to the same group as vlasovite".

The two minerals can be described using geometrical repeat unit of cTr = 2T4 3T4 and topological repeat unit of cVr = 2V2 3V2.


Unique IdentifiersHide

Mindat ID:
53413
Long-form identifier:
mindat:1:1:53413:2

IMA Classification of KhurayyimiteHide

Classification of KhurayyimiteHide

9.BK.05

9 : SILICATES (Germanates)
B : Sorosilicates
K : Unclassified sorosilicates

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

Physical Properties of KhurayyimiteHide

Vitreous
Colour:
Colorless
Streak:
White

Chemistry of KhurayyimiteHide

Mindat Formula:
Ca7Zn4(Si2O7)2(OH)10 · 4H2O
Element Weights:
Element% weight
O39.979 %
Ca25.037 %
Zn23.339 %
Si10.026 %
H1.619 %

Calculated from ideal end-member formula.
O
Ca
Zn
Si
H

Crystallography of KhurayyimiteHide

Crystal System:
Monoclinic
Class (H-M):
2/m - Prismatic
Space Group:
P21/c
Setting:
P21/c
Cell Parameters:
a = 11.2450(8) Å, b = 9.0963(5) Å, c = 14.068(1) Å
β = 113.237(8)°
Ratio:
a:b:c = 1.236 : 1 : 1.547
Unit Cell V:
1,322.26 ų (Calculated from Unit Cell)
Z:
2
Comment:
by Synchrotron Single-Crystal X-ray Diffraction

X-Ray Powder DiffractionHide

Geological EnvironmentHide

Paragenetic Mode(s):
Paragenetic ModeEarliest Age (Ga)
Stage 10a: Neoproterozoic oxygenation/terrestrial biosphere<0.6
51 : Pyrometamorphic minerals (see also #54 and #56)<0.36

Type Occurrence of KhurayyimiteHide

General Appearance of Type Material:
Spherulitic aggregates up to 200-300 μm in size. Individual elongated platy crystals in spherules are nearly 50 μm long and up to 10 μm thick.
Place of Conservation of Type Material:
Collections of the Fersman Mineralogical Museum, Russian Academy of Sciences, Leninskiy Prospekt 18-2, Moscow 119071, Russia, registration number 5298/1
Geological Setting of Type Material:
Small cavities and veins in altered spurrite marbles

Other Language Names for KhurayyimiteHide

Common AssociatesHide

Associations Based on Photo Data:
2 photos of Khurayyimite associated with CalciteCaCO3
1 photo of Khurayyimite associated with CuspidineCa8(Si2O7)2F4
1 photo of Khurayyimite associated with EttringiteCa6Al2(SO4)3(OH)12 · 26H2O
1 photo of Khurayyimite associated with SpurriteCa5(SiO4)2(CO3)

Other InformationHide

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 KhurayyimiteHide

References for KhurayyimiteHide

Localities for KhurayyimiteHide

Showing 1 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.
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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.
Jordan (TL)
 
  • Amman Governorate
    • Transjordan Plateau
      • Daba-Siwaqa complex
Galuskina et al. (2019) +1 other reference
 
and/or  
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