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Comparative Analysis of the Sverdrup and East Barents Sedimentary Basins


Дәйексөз келтіру

Толық мәтін

Ашық рұқсат Ашық рұқсат
Рұқсат жабық Рұқсат берілді
Рұқсат жабық Тек жазылушылар үшін

Аннотация

A comparative analysis of two large Arctic sedimentary basins was performed: the Sverdrup and East Barents, with emphasis on the quantitative parameters of sedimentation in the Mesozoic, determined by A.B. Ronov’s volumetric method. The similarities and differences of both basins are revealed, in particular, in sediment accumulation areas, in masses of sedimentary material per time unit, and in gross sand ratio. It was concluded that at the end of the Paleozoic and in the Mesozoic, both basins were close to each other but did not merge into one structure. In the Cenozoic, the distance between the basins increased due to spreading of the Eurasian Basin.

Авторлар туралы

M. Levitan

Vernadsky Institute of Geochemistry and Analytical Chemistry, Russian Academy of Sciences

Хат алмасуға жауапты Автор.
Email: m-levitan@mail.ru
Ресей, Moscow, 119334

T. Antonova

Vernadsky Institute of Geochemistry and Analytical Chemistry, Russian Academy of Sciences

Email: m-levitan@mail.ru
Ресей, Moscow, 119334

L. Domaratskaya

Vernadsky Institute of Geochemistry and Analytical Chemistry, Russian Academy of Sciences

Email: m-levitan@mail.ru
Ресей, Moscow, 119334

A. Koltsova

Vernadsky Institute of Geochemistry and Analytical Chemistry, Russian Academy of Sciences

Email: m-levitan@mail.ru
Ресей, Moscow, 119334

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