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Reconstruction of crystallisation temperature of artificially grown H-analcimes by means of the IR and fluid inclusion studies

Identyfikatory
Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
A method of reconstruction of the crystallisation temperature (Tc) of analcime has been proposed. The method is based on the compilation of two data sets: the IR absorption spectra and fluid inclusion study results. The water position in the analcime structure depends on the crystallisation temperature. Certain bands in the IR absorption spectrum are sensitive to the change in the temperature conditions of the analcime formation. Moreover, the IR absorption band positions are also influenced by the composition of the crystallisation system as well as by the crystallisation time. For more precise information about Tc, fluid inclusion studies were performed. They provide additional data about salt concentrations in the crystallisation system, water behaviour in the analcime structure and crystallisation temperature.
Rocznik
Strony
385--394
Opis fizyczny
Bibliogr.13 poz., il., tab.
Twórcy
autor
  • Institute of Geochemistry, Mineralogy and Petrology of the University, Warsaw, Poland
  • Institute of Geochemistry, Mineralogy and Petrology of the Warsaw University, Warsaw, Poland
Bibliografia
  • 1. BAKAKIN, V.V. 2001. On structure-genetic crystal chemistry of zeolites. In „Crystallogenesis and Mineralogy”, pp 34-35. St.Petersburg.
  • 2. BAKAKIN, V.V. 2001, in press. Isodimorphism of templates in zeolites. New crystal chemistry of analcime and its analogues. In: Proceedings of the 13th International Zeolite Conference, Series Studies in Surface Science and Catalisis, Elsevier; Amsterdam.
  • 3. BUKHAREV, V. P., GOSTYAEVA, N. M., NAUMENKO, V. V. & SHEMYAKINA, T. I. 1981. Temperature conditions of formation of ore and metasomatite minerals of the skarn-magnetite deposit Blagodat’ Mt. (Middle Urals). Geokhimiya i Rudoobrazovaniye, 9, 29-36. [In Russian]
  • 4. CERMIGNANI, C. & ANDERSON, G. M. 1983. The plagioclase exchange reaction in carbonate solution in carbonate solutions and application to nephelinisation. American Journal of Science, 283-A, 314-327.
  • 5. DE VIVO, B. & SASADA, M. 1992. Fluid inclusions in deep borehole SN-7D, Sumikawa geothermal field, Sengan area, Northeast Honsiu, Japan. J. Geoth. Res. Soc. Japan, 14 (2), 101-113.
  • 6. DOROSHENKO, YU. P., IVANOV V. N., PATRUSHEVA, M. A. & CHUMACHENKO N. M. 1969. Apophyllite from the polymetallic occurrence Savinskoye No. 5 (Transbaikalia). Mineralogitcheski Sbornik, 23 (4), 424-428. [In Russian]
  • 7. LISITSYN, A. YE. & RUDNEV, V. V. 1978. Certain physico-chemical conditions of formation of borosilicates in skarns. In: N. P. ERMAKOV (Ed.), Theory and practice in thermobarogeochemistry, pp. 139-142. Nedra; Moskva. [In Russian]
  • 8. ROEDDER, E. 1984. Fluid inclusions. Reviews in mineralogy, 12, 644 pp. Mineralogical Society of America; Washington.
  • 9. SŁABY E. 1999. Indicative significance of water environment in zeolitic structure – a study using experimentally grown cancrinite and analcime. Acta Geologica Polonica, 49, 25-65.
  • 10. SŁABY E. 2001a. Does the water environment point to the crystal symmetry? – a case study of artificially grown H-analcime. Mineralogia Polonica, Special Papers, 19, 162-164.
  • 11. SŁABY E. 2001b. Water environment in artificially grown analcimes. In: Crystallogenesis and mineralogy, pp. 366-367. St. Petersburg.
  • 12. SŁABY, E., KOZŁOWSKI, A., CZERWOSZ, E., DIDUSZKO, R. & BANERJEE, A. 1995. Investigation of synthetic fluid inclusions in hydrothermal analcimes. Bol. Soc. Esp. Mineral., 18 (1), 235-236.
  • 13. TAKENOUCHI, S. 1988. Fluid inclusion study of the Doroyu geothermal area, Akita. J. Geoth. Res. Soc. Japan, 10 (4), 321-338.
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-article-BGPK-0379-2633
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