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

N. G. Izokh; M. V. Erina; O. T. Obut; N. Kh Abdiev; A. I. Kim; U. D. Rakhmonov

doi:10.1134/S0031030120020057

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

N. G. Izokh, M. V. Erina, O. T. Obut, N. Kh Abdiev, A. I. Kim, U. D. Rakhmonov

Результат исследования: Научные публикации в периодических изданиях › статья › рецензирование

1 Цитирования (Scopus)

Аннотация

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.

Язык оригинала	английский
Страницы (с-по)	149-156
Число страниц	8
Журнал	Paleontological Journal
Том	54
Номер выпуска	2
DOI	https://doi.org/10.1134/S0031030120020057
Состояние	Опубликовано - 1 мар. 2020

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10.1134/S0031030120020057

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Late Devonian Conodonts from the Zeravshan-Gissar Mountainous Area, Uzbekistan. / Izokh, N. G.; Erina, M. V.; Obut, O. T. и др.

В: Paleontological Journal, Том 54, № 2, 01.03.2020, стр. 149-156.

Результат исследования: Научные публикации в периодических изданиях › статья › рецензирование

TY - JOUR

T1 - Late Devonian Conodonts from the Zeravshan-Gissar Mountainous Area, Uzbekistan

AU - Izokh, N. G.

AU - Erina, M. V.

AU - Obut, O. T.

AU - Abdiev, N. Kh

AU - Kim, A. I.

AU - Rakhmonov, U. D.

PY - 2020/3/1

Y1 - 2020/3/1

N2 - 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.

AB - 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.

KW - conodonts

KW - Late Devonian

KW - Zeravshan-Gissar mountainous area

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DO - 10.1134/S0031030120020057

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

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