Refined δ 13 С trend of the Dal’nyaya Taiga series of the Ura uplift (Vendian, southern part of Middle Siberia)

S. V. Rud’ko; P. Yu. Petrov; A. B. Kuznetsov; A. V. Shatsillo; O. L. Petrov

doi:10.1134/S1028334X17120182

Refined δ¹³С trend of the Dal’nyaya Taiga series of the Ura uplift (Vendian, southern part of Middle Siberia)

Авторы: Rud’ko S.V.¹, Petrov P.Y.¹, Kuznetsov A.B.², Shatsillo A.V.³, Petrov O.L.¹
Учреждения:
1. Geological Institute
2. Institute of Precambrian Geology and Geochronology
3. Schmidt Institute of Physics of the Earth
Выпуск: Том 477, № 2 (2017)
Страницы: 1449-1453
Раздел: Geochemistry
URL: https://ogarev-online.ru/1028-334X/article/view/191679
DOI: https://doi.org/10.1134/S1028334X17120182
ID: 191679

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Аннотация

New data were obtained on δ¹³С_carb and δ¹⁸O variations in the sequence of deposits of the Dal’nyaya Taiga series at the western and eastern flanks of the Ura anticline. The summary δ¹³С curve was plotted in view of the correlation of sequence–stratigraphic data of the basin analysis. A series of positive anomalies was found within the succession. Alternatives for global chemostratigraphic correlation of the Dal’nyaya Taiga series of the Ura uplift were considered.