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10. Seznam citované a doporučené literatury

Benešová, Z., and Ďurišová, J., 1980, Plynokapalné uzavřeniny a jejich význam pro geologii: Praha, ÚÚG, 80 p.

Bodnar, R. J. (1994): Synthetic fluid inclusions: XII. The system H2O-NaCl. Experimental determination of the halite liquidus and isochores for a 40 wt% NaCl solution. Geochimica et Cosmochimica Acta 58: 1053-1063

Bodnar, R. J. (1993): Revised equation and table for determining the freezing point depression of H2O-NaCl solutions. Geochimica et Cosmochimica Acta 57: 683-684

Bodnar, R. J., Sterner, S. M., and Hall, D. L. (1989): Salty: A fortran program to calculate compositions of fluid inclusions in the system NaCl-KCl-H2O. Computers and Geosciences 15: 19-41

Bodnar, R. J., Binns, P. R., and Hall, D. L. (1989): Synthetic fluid inclusions – VI. Quantitative evaluation of the decrepitation behaviour of fluid inclusions in quartz at one atmosphere confining pressure. Journal of Metamorphic Geology 7: 229-242

Bodnar, R. J. (1983): A method of calculating fluid inclusion volumes based on vapor bubble diameteres and P-V-T-X properties of inclusion fluids. Economic Geology 78: 535-542

Bodnar, R. J., Burnham, C. W., and Sterner, S. M. (1985): Syntetic fluid inclusions in natural quartz. III. Determination of equilibrium properties in the system H2O-NaCl to 1000oC and 1500 bars. Geochimica et Cosmochimica Acta 49: 1861-1873

Bodnar, R. J., and Sterner, S. M. (1985): Synthetic fluid inclusions in natural quartz. II. Application to PVT studies. Geochimica et Cosmochimica Acta 49: 1855-1859

Bodnar, R. J., Reynolds, T. J., and Kuehn, C. A. (1985): Fluid inclusions systematics in epithermal systems, in Berger, B. R., and Bethke, P. M., eds., Economic Geology: New York, Society of Economic Geology, pp 73-97

Borisenko, A. S. (1977): Izučenije solevogo sostava rastvorov gazovožidkich vklučenij v mineralach metodom kriometrii. Gologija i Geofizika 8: 16-27. Novosibirsk

Bowers, T. S., and Helgeson, H. C. (1983): Calculation of the thermodynamic and geological consequences of nonideal mixing in the system H2O-CO2-NaCl on phase relations in geologic systems: Equation of state for H2O-CO2-NaCl fluids at high pressures and temperatures. Geochimica et Cosmochimica Acta 47: 1247-1275

Bowers, T. S., and Helgeson, H. C. (1983): Calculation of the thermodynamic and geochemical consequences of nonideal mixing in the system H2O-CO2-NaCl on phase relations in geologic systems: metamorphic equilibria at high pressures and temperatures. American Mineralogist 68: 1059-1075

Bowers, T. S., and Helgeson, H. C. (1985): Fortran programs for generating fluid inclusion isochores and fugacity coefficients for the system H2O-CO2-NaCl at high pressures and temperatures. Computers and Geosciences 11: 203-213

Bowers, T. S. (1991): The deposition of gold and other metals: Pressure-induced fluid immiscibility and associated stable isotope signatures. Geochimica et Cosmochimica Acta 55: 2417-2434

Brown, P. E., and Lamb, W. M. (1989): P-V-T prpeties of fluids in the sysytem H2O+/-CO2+/-NaCl: New graphical presentations and implications for fluid inclusions studies. Geochimica et Cosmochimica Acta 53: 1209-1221

De Vivo, B., and Frezzotti, M. L., 1995, Fluid inclusions in minerals: Methods and applications: Blacksburg, Virginia Polytechnic Institute and State University, 377 pp. Objednat ji lze na adrese: bubbles@vt.edu za 25 US$.

Diamond, L. W. (1992): Stability of CO2 clathrate hydrate + CO2 liquid + CO2 vapour + aqueous KCl-NaCl solutions: Experimental datermination and application to salinity estimates of fluid inclusions. Geochimica et Cosmochimica Acta 56: 273-280

Ďurišová, J., and Hurai, V. (1991): Fluid inclusions in minerals (in Czech): Praha, Academia, 105 p.

Goldstein, R. H., and Reynolds, T. J. (1994): Systematics of fluid inclusions in diagenetic minerals, 199 pp.

Hollister, L. S., and Crawford, M. L. (1981) Fluid inclusions: Applications to petrology, MAC Short Course Volume 6, Mineralogical Association of Canada, p. 304.

Parnell, J. (1994): Geofluids: Origin, migration and evolution of fluids in sedimentary basins, Geol. Soc. London.

Roedder, E. (1984): Fluid inclusions, Mineralogical Society of America, 646 p.

Shepherd, T. J., Rankin, A. H., and Alderton, D. H. M. (1985): A practical guide to fluid inclusion studies: Glasgow and London, Blackie, 239 p.

Sterner, S. M., Hall, D. L., and Keppler, H. (1995): Compositional re-equilibration of fluid inclusions in quartz. Mineralogy and Petrology 119: 1-15

Sterner, S. M., and Bodnar, R. J. (1984): Synthetic fluid inclusions in natural quartz: I. Compositional types synthesized and applications to experimental geochemistry. Geochimica et Cosmochimica Acta 48: 2659-2668

Sterner, S. M., Hall, D. L., and Bodnar, R. J. (1988): Synthetic fluid inclusions. V. Solubility relations in the sysytem NaCl-KCl-H2O under vapour-saturated conditions. Geochimica et Cosmochimica Acta 52: 989-1005

Sterner, M. S., and Bodnar, R. J. (1989): The synthetic fluid inclusions – VII. Re-equilibration of fluid inclusions in quartz during laboratory-simulated metamorphic burial and uplift. Journal of Metamorphic Geology 7: 243-260

Sterner, S. M., and Bodnar, R. J. (1989): Synthetic fluid inclusions – VII. Re-equilibration of fluid inclusions in quartz during laboratory-simulated metamorphic burial and uplift. Journal of Metamorphic Geology 7: 243-260

Sterner, M. S., Chou, M. I., Downs, R. T., and Pitzer, K. S. (1992): Phase relations in the system NaCl-KCl-H2O: V. Thermodynamic-PTX analysis of solid-liquid equilibria at high temperatures and pressures. Geochimica et Cosmochimica Acta 56: 2295-2309

Sterner, S. M., Chou, I. M., Downs, R. T., and Pitzer, K. S. (1992): Phase relations in the system NaCl-KCl-H2O: V. Thermodynamic-PTX analysis of solid-liquid equilibria at high temperatures and pressures. Geochimica et Cosmochimica Acta 56: 2295-2309

Sterner, S. M., Hall, D. L., and Wheller, J. R. (1993): Post-entrapment compositional changes in synthetic and natural fluid inclusion: diffusional and re-equilibration of water. Archivum Mineralogiczne 49: 201-202

Sterner, M. S., Hall, D. L., and Keppler, H. (1995): Compositional re-equilibration of fluid inclusions in quartz. Mineralogy and Petrology 119: 1-15

Vityk, M. O., and Bodnar, R. J. (1995): Do fluid inclusions in high-grade metamorphic terranes preserve peak metamorphic density during retrograde decompression? American Mineralogist 80: 641-644

Vityk, M. O., and Bodnar, R. J. (1998): Statistical microthermometry of synthetic fluid inclusions in quartz during decompression reequilibration. Mineralogy and Petrology 132: 149 – 162

Zhang, Y. G., and Frantz, J. D. (1987): Determination of the homogenization temperatures and densities of supercritical fluids in the system NaCl-KCl-CaCl2-H2O using synthetic fluid inclusions. Chemical Geology 64: 335-350

Návrat na Obsah

11. Seznam použitých symbolů a zkratek

C.P. Kritický bod(critical point)
F Stupeň zaplnění 
H Halit NaCl
HH HydrohalitNaCl * 2 H2O
hm. % NaClekv. SalinitaVyjádření salinity pomocí NaCl ekvivalentu
I Led (Ice) 
L Kapalná fáze 
LAQ  Kapalná fáze bohatá H2O (v H2O - CO2 systému)
LCAR  Kapalná fáze bohatá CO2 (v H2O - CO2 systému)
P Tlak 
Pt  Tlak při vzniku inkluze
S Pevná fáze 
T nebo t Teplota 
Td teplota dekrepitaceTeplota při níž došlo k porušení inkluze
Te teplota eutektikateplota prvého rozeznatelného vzniku kapalné fáze v kompletně vymrazené inkluzi. Bývá též označována jako teplota prvého tání (first melting, TFM).
Th Teplota homogenizaceVždy je nutné blíže specifikovat jaká fáze homogenizuje a jakým způsobem (např.: L – na kapalinu, V-na plyn, C-kriticky)
Th-CO2  Teplota homogenizace CO2-fáze
Th-tot  Celková (konečná) teplota homogenizace
Tm Teplota táníAčkoli ve vodných nenasycených roztocích tato teplota znamená většinou tání ledu, v jiných případech tomu tak být nemusí. Proto se doporučuje vždy připojit označení fáze, která taje, či se rozpouští, např.: Tm-NaCl, Tm-ice, Tm-CO2 apod.
Tm-CLA Teplota tání klatrátůUrčuje se podle ní salinita v H2O - CO2 systému
Tm-CO2 Teplota tání pevného CO2 
Tm-h Teplota tání hydrátu 
Tm-ice Teplota tání ledu 
T.P. Trojný bod(triple point)
Ts Teplota rozpuštění dceřinného mineráluNapř. Ts-NaCl
Tt Teplota zachyceníTeplota při níž došlo ke vzniku inkluze (zachycení /uzavření/ fluida v inkluzi)
V Plynná fáze (pára) 
X Molární zlomekNapř. XCO2

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Autor: Jiří Zachariáš, Přírodovědecká fakulta Univerzity Karlovy v Praze