Late Devonian Conodonts from the Zeravshan-Gissar Mountainous Area, Uzbekistan

Late Devonian Conodonts from the Zeravshan-Gissar Mountainous Area, Uzbekistan

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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Veröffentlicht in:Paleontological journal 2020-03, Vol.54 (2), p.149-156
Hauptverfasser: Izokh, N. G., Erina, M. V., Obut, O. T., Abdiev, N. Kh, Kim, A. I., Rakhmonov, U. D.
Format: Artikel
Sprache:eng
Schlagworte:
Carbonate rocks
Carbonates
Devonian
Earth and Environmental Science
Earth Sciences
Geophysics
Mountain regions
Mountainous areas
Mountains
Paleontology
Surveys
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Zusammenfassung: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.
ISSN:0031-0301
1555-6174
DOI:10.1134/S0031030120020057