Standard

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.

Результаты исследований: Научные публикации в периодических изданиях › Обзорная статья › Рецензирование

Harvard

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)

APA

Baranskaya, A. V., Romanenko, F. A., Arslanov, H. A., Maksimov, F. E., Starikova, A. A., & Pushina, Z. V. (2018). Perennially frozen deposits of bely Island: Stratigraphy, age, depositional environments. Earth's Cryosphere, 22(2), 3-15. https://doi.org/10.21782/KZ1560-7496-2018-2(3-15)

Vancouver

Baranskaya AV, Romanenko FA, Arslanov HA, Maksimov FE, Starikova AA, Pushina ZV. Perennially frozen deposits of bely Island: Stratigraphy, age, depositional environments. Earth's Cryosphere. 2018 Янв. 1;22(2):3-15. https://doi.org/10.21782/KZ1560-7496-2018-2(3-15)

Author

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.

BibTeX

@article{80fb57c1b2b048ccb9dfdbca5f0bb43c,
title = "Perennially frozen deposits of bely Island: Stratigraphy, age, depositional environments",
abstract = "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.",
keywords = "Bely Island, Holocene, Pleistocene, Quaternary sediments, Sea level, Stratigraphy, Vertical movements of the Earth's crust",
author = "Baranskaya, {A. V.} and Romanenko, {F. A.} and Arslanov, {H. A.} and Maksimov, {F. E.} and Starikova, {A. A.} and Pushina, {Z. V.}",
year = "2018",
month = jan,
day = "1",
doi = "10.21782/KZ1560-7496-2018-2(3-15)",
language = "English",
volume = "22",
pages = "3--15",
journal = "КРИОСФЕРА ЗЕМЛИ",
issn = "1560-7496",
publisher = "Российская академия наук",
number = "2",

}

RIS

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

UR - http://www.scopus.com/inward/record.url?scp=85049199626&partnerID=8YFLogxK

U2 - 10.21782/KZ1560-7496-2018-2(3-15)

DO - 10.21782/KZ1560-7496-2018-2(3-15)

M3 - Review article

AN - SCOPUS:85049199626

VL - 22

SP - 3

EP - 15

JO - КРИОСФЕРА ЗЕМЛИ

JF - КРИОСФЕРА ЗЕМЛИ

SN - 1560-7496

IS - 2

ER -

ID: 35954975