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Ivanyukite-Na-T
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| Formula: |
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| System: | Trigonal | Colour: | Colorless to pale brown | |||||||||||||||||||||||||
| Hardness: | 4 | |||||||||||||||||||||||||||
| Name: | Named in honor of Gregory Yur’evich Ivanyuk, Russian mineralogist and petrologist, head of the Laboratory of Self-Organized Mineral Systems in the Geological Institute of the Kola Science Centre of the Russian Academy of Sciences | |||||||||||||||||||||||||||
This page provides mineralogical data about Ivanyukite-Na-T.
Classification of Ivanyukite-Na-T | ||||||||||||||||||||||||||
| IMA status: | Approved 2007 | |||||||||||||||||||||||||
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| mindat.org URL: | http://www.mindat.org/min-39652.html Please feel free to link to this page. | |||||||||||||||||||||||||
Type Occurrence of Ivanyukite-Na-T | ||||||||||||||||||||||||||
| Type Locality: | Koashva Mt, Khibiny Massif, Kola Peninsula, Murmanskaja Oblast', Northern Region, Russia | |||||||||||||||||||||||||
| Geological Setting of type material: | Ivanyukite-Na-T is a low-temperature hydrothermal mineral crystallized from supersaturated Na-rich aqueous solutions | |||||||||||||||||||||||||
Physical Properties of Ivanyukite-Na-T | ||||||||||||||||||||||||||
| Lustre: | Vitreous | |||||||||||||||||||||||||
| Diaphaneity (Transparency): | Transparent | |||||||||||||||||||||||||
| Colour: | Colorless to pale brown | |||||||||||||||||||||||||
| Streak: | White | |||||||||||||||||||||||||
| Hardness (Mohs): | 4 | |||||||||||||||||||||||||
| Cleavage: | Perfect on {1011} | |||||||||||||||||||||||||
| Density (measured): | 2.7 g/cm3 | |||||||||||||||||||||||||
| Density (calculated): | 2.384 g/cm3 | |||||||||||||||||||||||||
Crystallography of Ivanyukite-Na-T | ||||||||||||||||||||||||||
| Crystal System: | Trigonal | |||||||||||||||||||||||||
| Class (H-M): | 3m - Ditrigonal Pyramidal | |||||||||||||||||||||||||
| Space Group: | R3m | |||||||||||||||||||||||||
| Cell Parameters: | a = 10.921(3) Å, c = 13.885(4) Å | |||||||||||||||||||||||||
| Ratio: | a:c = 1 : 1.271 | |||||||||||||||||||||||||
| Unit Cell Volume: | V 1,434.17 ų (Calculated from Unit Cell) | |||||||||||||||||||||||||
| Z: | 3 | |||||||||||||||||||||||||
Optical Data of Ivanyukite-Na-T | ||||||||||||||||||||||||||
| Type: | Uniaxial (+) | |||||||||||||||||||||||||
| RI values: | nω = 1.760() nε = 1.850(9) | |||||||||||||||||||||||||
| Maximum Birefringence: | δ = 0.090 Chart shows birefringence interference colour range (at 30µm thickness) and does not take into account mineral colouration. | |||||||||||||||||||||||||
| Surface Relief: | Very High | |||||||||||||||||||||||||
Chemical Properties of Ivanyukite-Na-T | ||||||||||||||||||||||||||
| Formula: |
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| Essential elements: | H, Na, O, Si, Ti | |||||||||||||||||||||||||
| All elements listed in formula: | H, Na, O, Si, Ti | |||||||||||||||||||||||||
Other Names for Ivanyukite-Na-T | ||||||||||||||||||||||||||
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Other Information | ||||||||||||||||||||||||||
| Health Warning: | No information on health risks for this material has been entered into the database. You should always treat mineral specimens with care. | |||||||||||||||||||||||||
References for Ivanyukite-Na-T | ||||||||||||||||||||||||||
| Reference List: - + | Victor N. Yakovenchuk, Alexander P. Nikolaev, Ekaterina A. Selivanova, Yakov A. Pakhomovsky, Julia A. Korchak, Dar’ya V. Spiridonova, Oleg A. Zalkind, and Sergey V. Krivovichev (2009): Ivanyukite-Na-T, ivanyukite-Na-C, ivanyukite-K, and ivanyukite-Cu: New microporous titanosilicates from the Khibiny massif (Kola Peninsula, Russia) and crystal structure of ivanyukite-Na-T. American Mineralogist, 94, 1450–1458. | |||||||||||||||||||||||||
Internet Links for Ivanyukite-Na-T | ||||||||||||||||||||||||||
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Localities for Ivanyukite-Na-T | ||||||||||||||||||||||||||
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(TL) indicates type locality. ? indicates mineral may be doubtful at this locality. All other localities listed without reference should be considered as uncertain and unproven until references can be found.
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Locality Updated: Martin & Walling Mine, Mariposa Co., California, USAFrom Chester S. Lemanski, Jr., 24th May 2013 14:44:26

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