Reference Type | Journal (article/letter/editorial) |
---|
Title | Eringaite, Ca3Sc2(SiO4)3, a new mineral of the garnet group |
---|
Journal | Mineralogical Magazine |
---|
Authors | Galuskina, I. O. | Author |
---|
Galuskin, E. V. | Author |
Lazic, B. | Author |
Armbruster, T. | Author |
Dzierżanowski, P. | Author |
Prusik, K. | Author |
Wrzalik, R. | Author |
Year | 2010 (April) | Volume | 74 |
---|
Page(s) | 365-373 | Issue | 2 |
---|
Publisher | Mineralogical Society |
---|
Download URL | https://rruff.info/rruff_1.0/uploads/MM74_365.pdf+ |
---|
DOI | doi:10.1180/minmag.2010.074.2.365Search in ResearchGate |
---|
Classification | Not set | LoC | Not set |
---|
Mindat Ref. ID | 244072 | Long-form Identifier | mindat:1:5:244072:3 |
---|
|
GUID | d8f606b3-02dd-4113-942c-217017409c05 |
---|
Full Reference | Galuskina, I. O., Galuskin, E. V., Lazic, B., Armbruster, T., Dzierżanowski, P., Prusik, K., Wrzalik, R. (2010) Eringaite, Ca3Sc2(SiO4)3, a new mineral of the garnet group. Mineralogical Magazine, 74 (2) 365-373 doi:10.1180/minmag.2010.074.2.365 |
---|
Plain Text | Galuskina, I. O., Galuskin, E. V., Lazic, B., Armbruster, T., Dzierżanowski, P., Prusik, K., Wrzalik, R. (2010) Eringaite, Ca3Sc2(SiO4)3, a new mineral of the garnet group. Mineralogical Magazine, 74 (2) 365-373 doi:10.1180/minmag.2010.074.2.365 |
---|
In | (2010, April) Mineralogical Magazine Vol. 74 (2) Mineralogical Society |
---|
Abstract/Notes | Eringaite, Ca3Sc2(SiO4)3, a new mineral of the garnet group, is an accessory mineral in metasomatic rodingite-like rocks from the Wiluy River, Sakha-Yakutia Republic, Russia. Eringaite forms regular growth zones and irregular spots in complex garnet crystals containing a kimzeyite core. An electron back-scatter diffraction pattern with an excellent match to a garnet model with a = 12.19 Å was obtained for a grain with the largest Sc2O3 content having the crystal chemical formula (Ca2.98Y0.01Mg0.01)Σ3(Sc0.82Ti4+0.44Fe3+0.30Zr0.21Mg0.10Al0.09Cr3+0.08Fe2+0.05V3+0.01)Σ2.01(Si2.48Al0.30Fe3+0.22)Σ3O12. Eringaite is light brown to yellow with a creamy white streak. The crystals are transparent with a vitreous lustre. The calculated density of eringaite is 3.654 g cm–3. The following main modes of the Raman spectrum are characteristic of eringaite: 335, 511, 735, 880 and 937 cm–1. The strongest lines of the calculated powder diffraction data are as follows [(hkl) dhkl (I)] (400) 3.064 (69), (420) 2.740 (100), (422) 2.502 (68), (640) 1.670 (30), (642) 1.638 (82), (840) 1.370 (20), (842) 1.137 (19), (10.4.2) 1.119 (29). |
---|
These are possibly similar items as determined by title/reference text matching only.