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Anhydrite is widespread in the Prypiać Trough in the form of beds and nodules in the Subsaliferous Terrigenous and Carbonate formations (Eifelian and Frasnian), the Lower Saliferous Formation (Frasnian), the Intersaliferous and Upper Saliferous formations (Famennian). It is also present in the Asselian and Sakmarian (Lower Permian) deposits of the trough. The anhydrite is grey, blue, pink and orange. It has massive and, more rarely, horizontal bedding, and a fine- and micro-crystalline structure. Gypsum extends widely across the Orša Depression, Žlobin and Latvijas Saddles and partly in the Belarusian Anteclise, where it lies within the Eifelian deposits. It is also found in the Frasnian strata of the North-Prypiać Shoulder. As a component of facial analogue of the Upper Saliferous Formation gypsum forms the Bryniou deposit in the west of the Prypiać Trough. This mineral is also observed in the Oversaliferous Formation (Famennian) and in the Asselian and Sakmarian strata of the trough. There are spar, saccharoidal, alabastrine and selenitic varieties of gypsum. A medium to coarse crystalline structure is typical. The gypsum is grey, pink, yellow or orange.
Czasopismo
Rocznik
Tom
Strony
577–590
Opis fizyczny
Bibliogr. 35 poz., rys., tab.
Twórcy
autor
- Research and Production Centre for Geology, Academician Kuprevich 7, 220141 Minsk, Belarus
autor
- Research and Production Centre for Geology, Academician Kuprevich 7, 220141 Minsk, Belarus
autor
- Research and Production Centre for Geology, Academician Kuprevich 7, 220141 Minsk, Belarus
autor
- Research and Production Centre for Geology, Academician Kuprevich 7, 220141 Minsk, Belarus
Bibliografia
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- 21. Makhnach, A.S., Garetskiy, R.G., Matveev, A.V., Anoshko, Ya.I., eds., 2001. Geologiya Belarusi (in Russian). IGN NAN Belarusi. Minsk.
- 22. Moskvich, V.A., Konischev, V.S., 1986. Organogennye postroyki verkhnefamenskoy solenosnoy formatsii Pripyatskogo progiba (in Russian). In: Novye dannye po geologii solenosnykh basseynov Sovetskogo Soyuza (eds. A.L. Yanshin and G.A. Merzliakov): 94-101. Nauka, Moskva.
- 23. Obrovets, S.M., Vysotskiy, E.A., Kislik, V.Z., 1990. Litologo-fatsialnoye rayonirovaniye kalienosnoy subformatsii Pripyatskogo progiba (in Russian). In: Usloviya obrazovaniya mestorozhdeniy kaliynykh soley (eds. G.A. Merzliakov and M.A. Zharkov): 125-132. Nauka, Novosibirsk.
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- 27. Pozniakevich, Z.L., 1974. Stratigrafiya, osobennosti stroeniya i istoriya osadkonakopleniya piarnusko-narovskikh otlozheniy eifelskogo yarusa Pripyatskoy vpadiny (in Russian). In: Nekotorye voprosy stratigrafii i paleontologii paleozoyskikh i mezozoyskikh otlozheniy Belorusi (ed. V.K. Golubtsov): 8-68. BelNIGRI, Minsk.
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- 31. Uriev, 1.1., Anpilogov, A.P., 1977. Podsolevoy devon Pripyatskoy vpadiny (regionalnye zakonomernosti stroeniya i sostava) (in Russian). Nauka i Tekhnika, Minsk.
- 32. Vysotskiy, E.A., Kruchek, S.A., 2000. Stratigrafiya i obstanovki nakopleniya permskikh evaporitov Pripyatskogo progiba (in Russian). In: Problemy formirovaniya i kompleksnogo osvoeniya mestorozhdeniy solej. Tezisy dokladov VI solevogo soveschaniya (ed. A.I. Kudriashov): 44-46. Gornyy Institute UrO RAN, Solikamsk.
- 33. Vysotskiy, E.A., Garetskiy, R.G., Kislik, V.Z., 1988. Kalienosnye basseyny mira (in Russian). Nauka i Tekhnika, Minsk.
- 34. Vysotskiy, E.A., Makhnach, A.A., Peryt, T.M., Kruchek, S.A., 2004. Marine and continental Lower Permian evaporites of the Prypiac'Trough (Belarus). Sedimentary Geology, 172: 211-222.
- 35. Yarzhemskiy, J.J., 1960. K petrografii Belorusskogo solianogo mestorozhdeniya (in Russian). Trudy VNIIG, 40: 307-321.
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-ed940e10-43fb-4527-a12b-8697b776997b