Late Devonian Conodonts from the Zeravshan-Gissar Mountainous Area, Uzbekistan
Н. Г. ИзохTrofimuk Institute of Petroleum Geology and Geophysics, Siberian Branch, Russian Academy of Sciences, 630090, Novosibirsk, RussiaM. V. ErinaRegional Geological Survey, State Committee for Geology of the Republic of Uzbekistan, Tashkent, UzbekistanO.T. ObutTrofimuk Institute of Petroleum Geology and Geophysics, Siberian Branch, Russian Academy of Sciences, 630090, Novosibirsk, RussiaNuriddin AbdievA. I. KimRegional Geological Survey, State Committee for Geology of the Republic of Uzbekistan, Tashkent, UzbekistanUtkyr Rakhmonov
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Late Devonian conodonts, recovered from the siliceous and carbonate rocks of the upper part of the Akbasay Formation on the left side of the Kule Gorge, Zeravshan-Gissar mountainous area (Uzbekistan), are studied. Seven conodont associations are defined for the Frasnian–Famennian interval.
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