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Solubilities of anthracene, fluoranthene and pyrene in organic solvents: Mining , Brisbane, Austra- lia, 17 pp. In Audio without Methods. Phase equilibria in carbonic systems and their application to freezing studies of fluid inclusions. Click here to sign up. Dahlenborg L. Acta Geographica Lodziensia, 80,
CO2 was identified by measuring its triple point temperature Identification of the methane filling was made also on the basis of its triple point temperature All the cooling runs were made in a carefully dried-atmosphere box to avoid the covering of the cooling stage windows by hoar-frost. The bulk XCH4 values in the carbon dioxide-methane inclusions were determined by the final melting temperature of CO2 and the degree of filling by liquid at this temperature, as proposed by Swanenberg The H2O-CO2-salt inclusions were examined on the background of the results obtained by Gehrig and those of the H2O-CH4-salt type were compared to the experimental data published by Krader The plots of isochores for aqueous solutions were prepared on the basis of the tables published by Haas Jr.
Pressure was evaluated by the crossed isochores method Kalyuzhnyi and Koltun , see also Roedder and Bodnar for the aqueous solution — carbon dioxide inclusion pairs. For determinations of the solution concentration as the NaCl equivalent the curve proposed by Bodnar was used. Hydrogen sulfide in the inclusions was identified by its triple point temperature in the range of Three kinds of the inclusions were found, as characterized below.
All the considered inclusions homogenized in liquid phase. The temperatures given for aqueous inclusions are pressure-corrected on the basis of the crossed isochores method determinations and analysis of the appropriate systems. Group 1. Aqueous inclusions Fig. The eutectic points had temperature ca. CaCl2 Group 2. Aqueous inclusions, occasionally with CO2 separate phase, accompanied by rare inclusions filled by pure CO2 Fig.
The total salt concentration varied from 7. The determined components had concentrations: MgCl2 5. Group 3. Rare pure CO2 inclusions homogenized at How- ever, the carbon dioxide inclusions still homogenized in liquid phase. All were originally filled by liquid fluid; few of the associated inclusions, which homogenized in gaseous phase, were clearly separated parts of the larger necked-down inclusions and were not considered further. NaCl 4. These inclusions coexist with quite abundant CO2 inclusions with low admixture of CH4 not exceeding 0.
These carbonic inclusions homogenized in liquid phase at Aqueous inclusions bearing so- lution of elevated salinity, visually evide- nced by small square daughter crystals of halite ca. Total salt con- centrations were from In the sodic fluids NaCl concentration was The calcium-bearing fluid conta- ined 26, Inclusions of carbon dioxide with methane Fig. The mole fractions varied from 0. Micro-Raman spectrum of the H2S Group 4. Inclusions of hydrogen sulfide with inclusion, showing admixture of CH4.
Their melting temperature was The com-position of the inclusion filling was checked by its micro-Raman spectrum Fig. Results of the fluid inclusion studies are in agreement with the above conclusion. Each pulse started from higher pressure and then the pressure gradually decreased, but the decrease interval was relatively small. The low-temperature pulse caused most probably precipitation of gold. This is pertinent to the main inclusion group numbered one. Other two groups of inclusions filled by CO2-CH4 and H2S-CH4 marked important episodes associated with gold precipitation, but did not interrupt the main evolution of the mineral-forming fluid.
As it was written in the introduction, the area of finding of the native gold bearing pebbles was covered by gla- cial deposits transported there in Pleistocene from Sca- ndinavia. An attempt to attribute the gold bearing pebb- les to peculiar deposits in the source area was a very interesting experience. In the area of Fennoscandia the Fig.
Schematic paths of the in- amount of gold deposits and prospects exceeds one clusion fluids changes for the stu- hundred see e. Sundblad , thus the selection of died pebbles; the numbers refer to the acceptable parent one for the investigated speci- the inclusion groups see text. Significant part of them occurs in Finland Eilu et al.
Nevertheless, even in the area of Sweden still the number of the gold deposits remains large, and their new discoveries see e. Several types of gold deposits were recognized in Fennoscandia, namely iron oxide-copper gold Niiranen , metamorphosed copper porphyry Jakobsson et al. Characteristics of fluid inclusion assemblages are very good dist-inguishing features of the quartz specimens.
However, the set of the data for the Scandinavian gold deposits is not very extensive, though some basic information is obtainable from the published literature e.
The analysis of these data and comparison with the results of the studies performed on the gold-bearing pebbles from the Polish Baltic shore gave some interesting results. Though not exactly the same, the inclusion parameters are very similar, however, differences do exist. This may be explained by glacial erosion of shallower parts of the deposit than those sampled for the local study.
Nevertheless, similarities are undoubtedly numerous, thus this Swedish location may be evaluated as the tentatively determined source of the pebble. Hallberg Extent of the Mindel glacia- tion and possible sources of the gold- bearing pebbles, 1 — limits of the gla- cier, 2 — gold deposits, 3 — gold pro- spects, 4 — place of finding of the pe- bbles with native gold.
Bark , Bark et al.
The high pressure and continuous evolution of the mineral- forming fluids over a wide temperature range are especially significant. The fluid inclusions with halite daughter minerals gave similar temperature values of the daughter mineral dissolution and total inclusion filling homogenization both for the samples from the pebble and those from the deposit.
Simply the H2S inclusion filling is not trivial to distinguish and the identification requires special methods. Thus such inclusions may be in fact much frequent than it was reported till now.
The attempt to link the glacial pebbles bearing native gold found in the area of Poland with individual parent gold-ore deposits in Scandinavia resulted in a proposal which may be tentatively accepted, although more detailed studies of these deposits may yield more precise determinations. Probably a thorough search and investigation of the quartz pebbles in the southern Baltic Sea shores could result in sufficiently abundant samples for further comparisons. Nevertheless, a general opinions on Scandinavian gold accumulated in the glacial detritic deposits in Poland, especially in Lower Silesia, were already expressed earlier e.
Ack n ow le dge m e n t s I am very indebted to Dr. Textures and fluid inclusions in gold-bearing quartz veins, Falun, central Sweden; preliminary results. Stockholm Foerhandl. Ager D. Fenno-Scandian shield.
Ager Ed. Alioha P.
Alm E. Economic Geology, 98 7 , Amantov A. Plio-Pleistocene erosion of Fennoscandia and its implication for the Baltic area. Prace PIG, , Bark G.
Finland, Spec. Issue 1, Stockholm Foer- handl. Bejgarn T. Bergman J. Structural geology of Grundfors, a quartz vein related gold deposit in the Skell- efte district, northern Sweden. Bodnar R. Revised equation and table for determining the freezing point depression of H2O-NaCl solution. Acta, 57, — Bouchard M. Boulder transport in shield areas. Kujansuu, M. Sarni- sto Eds. Balkema, Rotterdam, Burruss R.
Analysis of phase equilibria in C-O-H-S fluid inclusions. Hollister, M. Crawford eds. Mineral Asso- ciation of Canada, Calgary, Crawford M. Phase equilibria in aqueous fluid inclusions. Craw- ford eds. Mineral Association of Canada, Calgary, Czubla P. Acta Geographica Lodziensia, 80, Eratyki przewodnie w glinach morenowych Polski. Dahlenborg L. DiLabio R. Glacial dispersal trains. Sarnisto Eds. Drake Resources Limited. Copper, gold and zinc in Sweden.
Mining , Brisbane, Austra- lia, 17 pp. Eilu P. A review of Gold mineralization styles in Finland. Gehrig M. HochschulVerlag Freiburg, pp. Goodwin R. Hydrogen sulfide provisional thermophysical properties from to K at pressures to 75 MPa. PB, pp. Harasimiuk, S. UMCS, Lublin, Narzutniaki skandynawskie — metodyka i interpretacja Scandinavian erratics — methods and interpretation. Rutkowski Eds.
Geologos, 14 2 , Landform Analysis, 12, Grodzicki A. Placer gold in Sudetes Mountains and in their foreland.
Gold in Poland, AM Monograph, 2, Gudelis W. Geologiczne, Warszawa, pp. Gumowska Z. Prace Mu- zeum Ziemi, 11, Pleistocene glaciation in Lithuania. Ehlers, P. Gibbard, P. Hughes Eds. Quaternary glaciations — extent and chronology, a closer look.
Developments in Quatrenary science, 15, Haas Jr. Physical properties of the coexisting phases and thermochemical properties of the H2O component in the boiling NaCl solutions. US Geol. Survey Bull. Thermodynamic properties of the coexisting phases and thermochemical pro- perties of the NaCl component in boiling NaCl solutions. Hallberg A. Mineralium Deposita, 29 2 , Hansen H.
Solubilities of anthracene, fluoranthene and pyrene in organic solvents: Solubility of fluoranthene in organic nonelectrolyte solvents. Comparison of observed versus predicted values based upon mobile order theory. Hesemann J. Geologische Rundschau, 22, Geologische Rundschau, 26, Kristalline Geschiebe der nordischen Vereisungen. Geologisches Landesamt Nordrhein-Westfalen, pp. Mertanen S. Whitehouse M. The series describes the adventures of 3 women: In politics he supports conservative Real Politics Union.
In Andrzej Pilipiuk under a pseudonym "Tomasz Olszakowski" also released 19 tomes continuing adventures about Pan Samochodzik:.
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