Polycyclic aromatic hydrocarbons in Holocene–Pleistocene sediments of the Laptev Sea

Polycyclic aromatic hydrocarbons in Holocene–Pleistocene sediments of the Laptev Sea

Bibliographic Details
Parent link:Doklady Earth Sciences
Vol. 468, iss. 1.— 2016.— [P. 496–499]
Corporate Authors: Национальный исследовательский Томский политехнический университет Институт природных ресурсов Кафедра геологии и разведки полезных ископаемых, Национальный исследовательский Томский политехнический университет Институт природных ресурсов Кафедра геологии и разведки полезных ископаемых Международная научно-образовательная лаборатория изучения углерода арктических морей
Other Authors: Drozdova A. N., Vetrov A. A., Romankevich E. A. Evgeny Aleksandrovich, Prokuda N. A., Sukhoverkhov S. V., Bratskaya S. Yu., Sergienko V. I., Semiletov I. P. Igor Petrovich, Ulyantsev A. S.
Summary:Title screen
The distribution and genesis of polycyclic aromatic hydrocarbons (PAHs) were studied in a 40-m core from a lagoon of the Laptev Sea that appeared during the Holocene resulting from the flooding of seawater into a freshwater lake in the area of the Buor-Khaya Gulf. The bulk of the core is constituted of permafrost rocks, thawed partially in their upper layers and covered with recent sediments (mainly by the products of intense thermoabrasion). The ratio of petrogenic and pyrogenic PAHs was evaluated.
Режим доступа: по договору с организацией-держателем ресурса
Published: 2016
Subjects:
электронный ресурс
труды учёных ТПУ
Online Access:http://dx.doi.org/10.1134/S1028334X16050123
Format: Electronic Book Chapter
KOHA link:https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=650290
Description
Summary:Title screen
The distribution and genesis of polycyclic aromatic hydrocarbons (PAHs) were studied in a 40-m core from a lagoon of the Laptev Sea that appeared during the Holocene resulting from the flooding of seawater into a freshwater lake in the area of the Buor-Khaya Gulf. The bulk of the core is constituted of permafrost rocks, thawed partially in their upper layers and covered with recent sediments (mainly by the products of intense thermoabrasion). The ratio of petrogenic and pyrogenic PAHs was evaluated.
Режим доступа: по договору с организацией-держателем ресурса
DOI:10.1134/S1028334X16050123

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