Alkanes in Quaternary deposits of the Laptev Sea


Дәйексөз келтіру

Толық мәтін

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

Аннотация

The distribution and genesis of n-alkanes in sediments from the 38-m sequence obtained during core boring in the Ivashkina lagoon were studied. Sediments were formed in the Holocene as a result of thermokarst and penetration of seawater. The sequence mostly includes permafrost rocks partially molten in the upper horizons and covered by Quaternary deposits, which are mostly the products of thermoabrasion.

Авторлар туралы

E. Romankevich

Shirshov Institute of Oceanology; Tomsk National Research Polytechnic University

Email: ratnick@mail.ru
Ресей, Moscow, 119991; Tomsk

A. Vetrov

Shirshov Institute of Oceanology

Email: ratnick@mail.ru
Ресей, Moscow, 119991

N. Belyaev

Shirshov Institute of Oceanology; Tomsk National Research Polytechnic University

Хат алмасуға жауапты Автор.
Email: ratnick@mail.ru
Ресей, Moscow, 119991; Tomsk

V. Sergienko

Institute of Chemistry, Far East Branch

Email: ratnick@mail.ru
Ресей, Vladivostok, 690022

I. Semiletov

Il’ichev Pacific Institute of Oceanology, Far East Branch; Tomsk National Research Polytechnic University

Email: ratnick@mail.ru
Ресей, Vladivostok, 690041; Tomsk

S. Sukhoverkhov

Institute of Chemistry, Far East Branch

Email: ratnick@mail.ru
Ресей, Vladivostok, 690022

S. Bratskaya

Institute of Chemistry, Far East Branch

Email: ratnick@mail.ru
Ресей, Vladivostok, 690022

N. Prokuda

Institute of Chemistry, Far East Branch

Email: ratnick@mail.ru
Ресей, Vladivostok, 690022

A. Ulyantsev

Shirshov Institute of Oceanology

Email: ratnick@mail.ru
Ресей, Moscow, 119991

Қосымша файлдар

Қосымша файлдар
Әрекет
1. JATS XML

© Pleiades Publishing, Ltd., 2017