Thermal stability and vibrational spectra of the sheet borate tuzlaite, NaCa[B5O8(OH)2]3H2O

American Mineralogist

Volumn 88, Issue 2-3, 2003, Pages 271-276

  Bermanec, Vladimir ^a   Furić, Krešimir ^b   Rajić, Maša ^c   Kniewald, Goran ^b  

^a UNIVERSITY OF ZAGREB   (Croatia)

^b RUDER BO KOVI INSTITUTE   (Croatia)

^c Brodarski Institut doo   (Croatia)

Author keywords

[No Author keywords available]

Indexed keywords

HYDRATION; MOLECULES; THERMOANALYSIS;

BOSNIA AND HERZEGOVINA; FORMATION PATHWAYS; H2O MOLECULES; HYDROXYL GROUPS; PHASE RELATIONSHIPS; SEQUENTIAL POLYMERIZATION; STRUCTURAL TRANSFORMATION; WATER MOLECULE;

BORATE MINERALS;

BORATE; CRYSTAL STRUCTURE; DEHYDRATION; PHASE TRANSITION; THERMAL STRUCTURE; TUZLAITE; WATER CONTENT; X-RAY DIFFRACTION;

EID: 0037293398     PISSN: 0003004X     EISSN: None     Source Type: Journal    
DOI: 10.2138/am-2003-2-303     Document Type: Article

References (13)

1. Anovitz, L.M. and Hemingway, B.S. (1996) Thermodynamics of boron minerals: summary of structural, volumetric and thermochemical data. In L.M. Anovitz and E.S. Grew, Eds., Boron: mineralogy, petrology and geochemistry, 33, 181-261. Reviews in Mineralogy, Mineralogical Society of America, Washington, D.C.
2. Armbruster, T., Bermanec, V., Wenger, M., and Oberhånsli, R. (1989) Crystal chemistry of double-ring silicates: structure of natural and dehydrated milarite at 100K. European Journal of Mineralogy, 1, 353-362.
3. Bermanec, V., Tibljaš, D., Crnjaković, M., and Kniewald, G. (1992) Saline minerals of the Tuzla salt deposit as indicators of palaeooceanographic conditions. Rapports de la Commission Internationale pour l'Exploration Scientifique de la Mer Méditerranee, 33, 116. Monaco, Principality of Monaco.
4. 2O, a new mineral with a pentaborate sheet structure from the Tuzla salt mine, Bosnia and Hercegovina. American Mineralogist, 79, 562-569.
5. Bermanec, V., Crnjaković, M., and Kniewald, G. (2001) Geochemistry and mineral assemblages of the Mediterranean evaporite deposits 3. Some textural characteristics of evaporite sediments in Tuzla salt deposit. Rapports de la Commission Internationale pour l'Exploration Scientifique de la Mer Méditerrance, 36, 9. Monaco, Principality of Monaco.
6. Burns, P.C., Grice, J.D., and Hawthorne, F.C. (1995) Borate minerals 1. Polyhedral clusters and fundamental building blocks. Canadian Mineralogist, 33, 1131-1151.
7. Farmer, V.C. (1974) The infrared spectra of minerals. Mineralogical Society Monograph 4, London. 539 p.
8. Hardie, L.A. and Eugster, H.P. (1971) The depositional environment of marine evaporites: a case for shallow, clastic accumulation, Sedimentology, 16, 187-220.
9. V. Svensk Kemisk Tidskrift, 75, 3-34.
10. Kniewald, G., Bermanec, V., and Tibljaš, D. (1986) On the origin and type of the Tuzla salt deposit in Yugoslavia. Rapports de la Commission Internationale pour l'Exploration Scientifique de la Mer Méditerrance, 30/2, 72. Monaco, Principality of Monaco.
11. Kniewald, G., Bermanec, V., and Tibljaš, D. (1995) The depositional environment of the evaporite mineral series at Tuzla, Bosnia-Hercegovina. Rapports de la Commission Internationale pour l'Exploration Scientifique de la Mer Méditerranee, 34, 105. Monaco. Principality of Monaco.
12. Smith, G.I. and Medrano, M.D. (1996) Continental borate deposits of Cenozoic age. In L.M.Anovitz and E.S.Grew, Eds., Boron: mineralogy, petrology and geochemistry, 33, 263-298. Reviews in Mineralogy, Mineralogical Society of America, Washington, D.C.
13. Warren, J. (1999) Evaporites-their evolution and economics. Blackwell Science, Oxford, 448 pages.