Fluorites inclusions

Fig. 4.4. a-d Laser-induced time-resolved luminescence spectra of apatite with uranyl (a-c) and luminescence (d) after oxidizing heating (possibly in fluorite inclusions)... 

Figure 7. Infrared spectrum, and chemical profiling hydrocarbon fluid inclusion in fluorite (inclusion A), (a) Typical infrared spectrum recorded with an aperture of 3 3 pm2, hemical profiling is reported for the band located at 3697 cm-1 attributed to hydroxyl (b), for the C02 band (c), and for the aliphatic compounds (d). [Used by permission of the Society for Applied Spectroscopy, from Guilhaumou et al. (1998), Appl Spectroscopy, Vol. 52, Fig. 3, p. 1031.]...

Fluorites inclusions, 869 Formaldehyde hydroformylation catalysts, rhodium complexes, 261 Forraamidinesulfinic acid technetium complexes, 974 Formate dehydrogenases bacteria... 

We mentioned in Section IV.C that ice-iiquid equiiibrium was observed up to 6.5°C in natural fluorite inclusions [63]. However, this work involved aqueous solutions of unknown composition and contained no corresponding study of high-temperature cavitation. 

Fluid inclusion studies have shown that basinal fluids responsible for depositing fluorite ore... 

Munoz M., Boyce A. L, Courjault-Rade P., Fallick A. E., and Tohon E. (1991) Continental basinal origin of ore veins from southwestern Massif Central fluorite veins (Albigeois, Erance) evidence for fluid inclusion and stable isotope analysis. Appl. Geochem. 14, 447-458. 

Roedder, E., 1967. Environment of deposition of stratiform (Mississippi Valley-type) ore deposits, from studies of fluid inclusions. In J.B. Brown (Editor), Genesis of Stratiform Lead-Zinc-Barite-Fluorite Deposits (Mississippi Valley-type Deposits). Econ. Geol. Monograph, 3 349—361. 

Fig. 1. (Continued) (E) Coarse-crystalline saddle dolomite replacing host dolomicrospar. Note optical zoning of dolospar due to variable inclusion densities. Triassic limestone with epigenetic dolomite and sphalerite-galena-fluorite mineralization. Eastern Alps (Wanneck area, Tyrol). Scale bar = 500 pm. (F) Host carbonate rock completely replaced by non-planar dolospar. Note that about half of the crystals in the field of view show regularly curved crystal boundaries and/or incipient sweeping extinction, i.e. saddle dolomite. Triassic limestone with epigenetic dolomite and sphalerite-galena-fluorite mineralization. Eastern Alps (Wanneck area, Tyrol). Scale bar = 500 pm. (See also colour Plate 1, facing p. 446.)...

Kendrick MA, Burgess R, Pattrick RAD, Turner G (2002a) The origin of a fluorite rich MVT brine combined noble gas (He, Ar, Kr) and halogen (Cl, Br, I) analysis of fluid inclusions from the South Pennine Orefield, U.K. Econ Geol (in press)... 

The formula, Rn02n-2, was used as the generic homologous series formula of the rare earth higher oxides for more than 30 years until Kang and Eyring established an all-inclusive formula, Rn02n-2m, based on the fluorite-type module theory. 

JI Koivula, S Elen. Barite Inclusions in fluorite. Gems Gemol 34 281-283, 1998. 

Microordering areas are about 10-100 nm long. It is impossible to detect these randomly oriented nanometric areas by means of classical XRD because both the fluorite matrix and ordered inclusions have an almost identical cationic sublattice. Slight cation displacements... 

Bird, B. C., and Darling, R. S. (1996). Fluid Inclusion Study of the Long Lake Calcite-Fluorite Vein, Central Adirondacks. Geol. Soc. Am., Abs. 28(3), 38 pp. 

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