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On the origin of chloride waters in the Polish Flysch Carpathians

Treść / Zawartość
Identyfikatory
Warianty tytułu
Konferencja
Groundwater quality sustainability : XXXVIII IAH Congress in Kraków
Języki publikacji
EN
Abstrakty
EN
Chloride waters in the Polish Flysch Carpathians are remnants of marine sedimentation water which was chemically and isotopically changed due to ultrafiltration and the release of dehydration water (diagenetic water) during the burial diagenesis of clay minerals. In the western part of the study area, the diagenetic end-member is characterized by δ18O and δ2H values of about +6.5 and –30.0‰, respectively, and Cl– content in the range of 3.8 and 13.8 g/dm3. In some fault areas, such waters migrate to the surface and mix with local meteoric waters as indicated by mixing lines in δ18O–δ2H and δ18O–Cl– graphs. In several wells of the eastern part, waters containing a significant proportion of marine water occur. However, in majority of deep wells, mixtures of diagenetic and meteoric waters of Quaternary and pre-Quaternary climates are present, as deduced from δ18O–Cl– linear relations. In most cases, they do not exhibit linear relations also expected in δ18O–δ2H graphs due to the shifts of δ2H to heavier isotopic values supposedly caused by involvement of water in the generation of hydrocarbons.
Rocznik
Strony
201--208
Opis fizyczny
Bibliogr. 17 poz., rys., wykr.
Twórcy
autor
  • Polish Geological Institute – National Research Institute, Carpathian Branch, Skrzatów 1, 31-560 Kraków, Poland
autor
  • Polish Geological Institute – National Research Institute, Carpathian Branch, Skrzatów 1, 31-560 Kraków, Poland
autor
  • Polish Geological Institute – National Research Institute, Carpathian Branch, Skrzatów 1, 31-560 Kraków, Poland
Bibliografia
  • 1. COPLEN T.B., HOPPLE J.A., BÖHLKE J.K., PEISER H.S., RIEDER S.E., KROUSE H.R., ROSMAN K.J.R., DING T., VOCKE R.D., RÉVÉSZ K.M., LAMBERTY A., TAYLOR P., De BIÈVRE P., 2002 — Compilation of minimum and maximum isotope ratios of selected elements in naturally occurring terrestrial materials and reagents. Water-Resources Investigations Report 01-4222. USGS, Reston.
  • 2. DOWGIAŁŁO J., 1980 — Polygenetic model of the Carpathian chloride waters and its some consequences. In: Współczesne problemy hydrogeologii: 275–290. UW, Warszawa [in Polish].
  • 3. DOWGIAŁŁO J., LEŚNIAK P.M., 1980 — The origin of chloride waters in the Polish Flysch Carpathians. In: Proc. 3rd Int. Symp. Water-Rock Interaction: 20–24. Edmonton.
  • 4. GOLONKA J., BORYSŁAWSKI A., PAUL Z., RYŁKO W., 1979 — Mapa geologiczna Polski 1:200 000, ark. Bielsko-Biała. Inst. Geol., Warszawa.
  • 5. HOWER J., ESLINGER E., HOWER M., PERRY E., 1976 — Mechanism of burial metamorphism of argillaceous sediment: 1. Mineralogical and chemical evidence. Geol. Soc. Am. Bull., 87: 725–737.
  • 6. LEŚNIAK P.M., 1980 — The origin of the chloride waters at Wysowa, West Carpathians – chemical and isotopic approach. Acta Geol. Pol., 30: 519–550.
  • 7. LONGSTAFFE F.J., 1987 — Stable isotope studies of diagenetic processes. In: Short Course in Stable Isotope Geochemistry of Low Temperature Fluids (ed. T.K. Kyser): 187–257. Mineralogical Association of Canada, Saskatoon.
  • 8. NIEŚCIERUK P., PAUL Z., RYŁKO W., SZYMAKOWSKA F., WÓJCIK A.,ŻYTKO K., 1995 — Mapa geologiczna Polski 1:200 000, ark. Jasło. Państw. Inst. Geol., Warszawa.
  • 9. OSZCZYPKO N., ZUBER A., 2002 — Geological and isotopic evidence of diagenetic waters in the Polish Flysch Carpathians. Geol. Carpath., 53, 4: 1–13.
  • 10. POROWSKI A., 2006 — Origin of mineralized waters in the Central Carpathian Synclinorium, SE Poland. Stud. Geol. Pol., 125: 5–67.
  • 11. RAJCHEL L., ZUBER A., DULINSKI M., RAJCHEL J., 2004 — Occurrences and genesis of chloride waters in Sól (S Poland). Prz. Geol. 52, 12: 1179–1186 [in Polish].
  • 12. ŚRODOŃ J., 2007 — Illitization of smectite and history of sedimentary basins. In: Invited Lectures of the 11th EUROCLAY Conference: 74–82. Aveiro, Portugal.
  • 13. ŚRODOŃ J., ELSASS F., McHARDY W.J., MORGAN D.J., 1992 — Chemistry of illite-smectite inferred from TEM measurements of fundamental particles. Clay Minerals, 27: 137–158.
  • 14. ŚWIERCZEWSKA A., 2005 — The interplay of the thermal and structural histories of the Magura Nappe (Outer Carpathians) in Poland and Slovakia. Miner. Pol., 36: 91–144.
  • 15. WHITE, D.E., BARNES, I., O'NEIL, J.R., 1973 — Thermal and mineral waters of nonmeteoric origin, California Coast Ranges. Geol. Soc. Am. Bull., 84: 547–560.
  • 16. ZUBER A., CHOWANIEC J., 2009 — Diagenetic and other highly mineralized waters in the Polish Carpathians. Appl. Geochem., 24: 1889–1900.
  • 17. ZUBER A., GRABCZAK J., 1985 — Origin of some mineral waters in southern Poland as deduced from isotope investigations. In: Aktualne problemy hydrogeologii: 135–148. Wyd. AGH, Kraków [in Polish].
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-6246ddf9-c7ae-469f-a31b-ebee9bec812c
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