Perennially frozen deposits of bely Island: Stratigraphy, age, depositional environments

A. V. Baranskaya, F. A. Romanenko, H. A. Arslanov, F. E. Maksimov, A. A. Starikova, Z. V. Pushina

Результат исследований: Научные публикации в периодических изданияхОбзорная статья

3 Цитирования (Scopus)

Выдержка

This paper is an overview of the study of perennially frozen deposits outcropping in the coastal cliffs of the western and eastern parts of Bely Island. The obtained results provide information about the composition, structure, stratigraphy, origin and age of Quaternary deposits. It has been established that the cross-section consists of three main units: the lower silts and clays formed during MIS 3 in the marine conditions; the middle sandy unit accumulated between 9 and 5 kA BP as a result of small-scale local relative sea level rise; the upper unit consisting of clays, loam, peat and aeolian sands of terrestrial origin formed in the Late Holocene.

Язык оригиналаанглийский
Страницы (с-по)3-15
Число страниц13
ЖурналEarth's Cryosphere
Том22
Номер выпуска2
DOI
СостояниеОпубликовано - 1 янв 2018

Отпечаток

clay loam
cliff
depositional environment
peat
stratigraphy
cross section
Holocene
clay
sand
sea level rise

Предметные области Scopus

  • Планетоведение и науки о земле (все)

Цитировать

Baranskaya, A. V. ; Romanenko, F. A. ; Arslanov, H. A. ; Maksimov, F. E. ; Starikova, A. A. ; Pushina, Z. V. / Perennially frozen deposits of bely Island : Stratigraphy, age, depositional environments. В: Earth's Cryosphere. 2018 ; Том 22, № 2. стр. 3-15.
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Baranskaya, AV, Romanenko, FA, Arslanov, HA, Maksimov, FE, Starikova, AA & Pushina, ZV 2018, 'Perennially frozen deposits of bely Island: Stratigraphy, age, depositional environments', Earth's Cryosphere, том. 22, № 2, стр. 3-15. https://doi.org/10.21782/KZ1560-7496-2018-2(3-15)

Perennially frozen deposits of bely Island : Stratigraphy, age, depositional environments. / Baranskaya, A. V.; Romanenko, F. A.; Arslanov, H. A.; Maksimov, F. E.; Starikova, A. A.; Pushina, Z. V.

В: Earth's Cryosphere, Том 22, № 2, 01.01.2018, стр. 3-15.

Результат исследований: Научные публикации в периодических изданияхОбзорная статья

TY - JOUR

T1 - Perennially frozen deposits of bely Island

T2 - Stratigraphy, age, depositional environments

AU - Baranskaya, A. V.

AU - Romanenko, F. A.

AU - Arslanov, H. A.

AU - Maksimov, F. E.

AU - Starikova, A. A.

AU - Pushina, Z. V.

PY - 2018/1/1

Y1 - 2018/1/1

N2 - This paper is an overview of the study of perennially frozen deposits outcropping in the coastal cliffs of the western and eastern parts of Bely Island. The obtained results provide information about the composition, structure, stratigraphy, origin and age of Quaternary deposits. It has been established that the cross-section consists of three main units: the lower silts and clays formed during MIS 3 in the marine conditions; the middle sandy unit accumulated between 9 and 5 kA BP as a result of small-scale local relative sea level rise; the upper unit consisting of clays, loam, peat and aeolian sands of terrestrial origin formed in the Late Holocene.

AB - This paper is an overview of the study of perennially frozen deposits outcropping in the coastal cliffs of the western and eastern parts of Bely Island. The obtained results provide information about the composition, structure, stratigraphy, origin and age of Quaternary deposits. It has been established that the cross-section consists of three main units: the lower silts and clays formed during MIS 3 in the marine conditions; the middle sandy unit accumulated between 9 and 5 kA BP as a result of small-scale local relative sea level rise; the upper unit consisting of clays, loam, peat and aeolian sands of terrestrial origin formed in the Late Holocene.

KW - Bely Island

KW - Holocene

KW - Pleistocene

KW - Quaternary sediments

KW - Sea level

KW - Stratigraphy

KW - Vertical movements of the Earth's crust

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M3 - Review article

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