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Jinshajiangite: structure, twinning and pseudosymmetry.
Shiyun Jin1, Huifang Xu1, Seungyeol Lee1
1Department of Geoscience, University of Wisconsin-Madison, 1215 W. Dayton Street, Madison, WI 53706, USA.
Summary
This study reveals the correct triclinic crystal structure of jinshajiangite, a titanium silicate mineral. This finding clarifies structural relationships among related minerals and corrects previous models.
Area of Science:
- Mineralogy
- Crystallography
- Materials Science
Background:
- Jinshajiangite is a titanium silicate mineral with a complex structure.
- Previous structural models for jinshajiangite and related minerals were based on inaccurate crystallographic data.
Purpose of the Study:
- To accurately determine the crystal structure of jinshajiangite using advanced analytical techniques.
- To clarify the structural relationships between jinshajiangite, perraultite, surkhobite, and bobshannonite.
- To propose a revised structural model for bafertisite.
Main Methods:
- Single-crystal X-ray diffraction
- Transmission electron microscopy
Main Results:
- The crystal structure of jinshajiangite was determined to be triclinic (P\bar 1 symmetry), with specific lattice parameters (a = 8.7331(2) Å, b = 8.7366(2) Å, c = 11.0404(3) Å, α = 81.477(1)°, β = 110.184(1)°, γ = 104.384(1)°).
- The determined structure differs significantly from the previously proposed monoclinic cell, featuring a single type of titanium silicate and cation layer.
- No significant iron-manganese ordering was observed despite high manganese content.
- All perraultite-type minerals share the P\bar 1 structure of jinshajiangite, with previously proposed monoclinic space groups attributed to polysynthetic twinning.
Conclusions:
- The study establishes the correct triclinic crystal structure for jinshajiangite.
- This revised understanding impacts the classification and structural interpretation of perraultite-group minerals.
- The findings provide a new polytype structure model for bafertisite, resolving structural ambiguities.
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