Alkanes in Quaternary deposits of the Laptev Sea

E. A. Romankevich, A. A. Vetrov, N. A. Belyaev, V. I. Sergienko, I. P. Semiletov, S. V. Sukhoverkhov, S. Yu Bratskaya, N. A. Prokuda, A. S. Ulyantsev

Результат исследований: Материалы для журналаСтатья

1 Цитирования (Scopus)

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.

Язык оригиналаАнглийский
Страницы (с-по)36-39
Число страниц4
ЖурналDoklady Earth Sciences
Том472
Номер выпуска1
DOI
СостояниеОпубликовано - 1 янв 2017

ASJC Scopus subject areas

  • Earth and Planetary Sciences (miscellaneous)
  • Earth and Planetary Sciences(all)

Fingerprint Подробные сведения о темах исследования «Alkanes in Quaternary deposits of the Laptev Sea». Вместе они формируют уникальный семантический отпечаток (fingerprint).

  • Цитировать

    Romankevich, E. A., Vetrov, A. A., Belyaev, N. A., Sergienko, V. I., Semiletov, I. P., Sukhoverkhov, S. V., Bratskaya, S. Y., Prokuda, N. A., & Ulyantsev, A. S. (2017). Alkanes in Quaternary deposits of the Laptev Sea. Doklady Earth Sciences, 472(1), 36-39. https://doi.org/10.1134/S1028334X17010093