Traces of the Tunguska Event (1908) in Sediments of Zapovednoe Lake Based on SR–XRF Data | Sciact - CRIS-система Института катализа

Traces of the Tunguska Event (1908) in Sediments of Zapovednoe Lake Based on SR–XRF Data Научная публикация

Журнал

Transactions (Doklady) of the Russian Academy of Sciences. Earth science sections (1992-1997) Continued by Doklady Akademii nauk. English. Doklady earth sciences ( 1028-334X )
ISSN: 1083-3552

Вых. Данные

Год: 2020, Том: 292, Номер: 2, Страницы: 442-445 Страниц : 4 DOI: 10.1134/S1028334X20060045

Ключевые слова

Tunguska event 1908, lake sediments, X-ray fluorescent analysis (XRF), synchrotron radiation (SR), microelements

Авторы

Darin A.V. ¹ , Rogozin D.Yu. ^2,3 , Meydus A.V. ⁴ , Babich V.V ¹ , Kalugin I.A. ¹ , Markovich T.I. ¹ , Rakshun Ya.V. ⁵ , Darin F.A. ⁵ , Sorokoletov D.S. ⁵ , Gogin A.A. ⁶ , Senin R.A. ⁶ , Degermendzhi A.G. ²

Организации

1	Sobolev Institute of Geology and Mineralogy, Siberian Branch, Russian Academy of Sciences, Novosibirsk, 630090 Russia
2	Institute of Biophysics, Siberian Branch, Russian Academy of Sciences, Krasnoyarsk, 660036 Russia
3	Siberian Federal University, Krasnoyarsk, 660041 Russia
4	Tungusskii State Nature Reserve, Krasnoyarsk, 648490 Russia
5	Budker Institute of Nuclear Physics, Siberian Branch, Russian Academy of Sciences, Novosibirsk, 630090 Russia
6	Kurchatov Institute National Research Center, Moscow, 123182 Russia

An anomalous layer enriched with chemical elements indicating the presence of terrigenous matter was discovered in the sediment core of Zapovednoe Lake located 60 km from the epicenter of the Tunguska event (1908) using synchrotron radiation X-ray fluorescence spectroscopy (SR–XRF). Radioisotope measurements indicate that the age of the layer is consistent with the date of the catastrophe. Apparently, the anomalous layer was formed as a result of an intense terrigenous matter inflow from the water catchment area due to massive forest falls and subsequent wildfires caused by the Tunguska event. Thus, it is established that targeted searches for microparticles of extraterrestrial origin can be carried out in the discovered and dated anomalous bottom sediment layer.

Darin A.V. , Rogozin D.Y. , Meydus A.V. , Babich V.V. , Kalugin I.A. , Markovich T.I. , Rakshun Y.V. , Darin F.A. , Sorokoletov D.S. , Gogin A.A. , Senin R.A. , Degermendzhi A.G.
Traces of the Tunguska Event (1908) in Sediments of Zapovednoe Lake Based on SR–XRF Data
Transactions (Doklady) of the Russian Academy of Sciences. Earth science sections (1992-1997) Continued by Doklady Akademii nauk. English. Doklady earth sciences ( 1028-334X ). 2020. V.292. N2. P.442-445. DOI: 10.1134/S1028334X20060045 WOS Scopus CAPlus OpenAlex

Дарьин А.В. , Рогозин Д.Ю. , Мейдус А.В. , Бабич В.В. , Калугин И.А. , Маркович Т.И. , Ракшун Я.В. , Дарьин Ф.А. , Сороколетов Д.С. , Гогин А.А. , Сенин Р.А. , Дегерменджи А.Г.
Следы тунгусского события 1908 г. в донных осадках озера Заповедное по данным сканирующего РФА-СИ
Доклады Российской академии наук. Науки о Земле. 2020. Т.492. №2. С.61-65. DOI: 10.31857/s2686739720060043 OpenAlex

Поступила в редакцию:	13 мар. 2020 г.
Принята к публикации:	3 апр. 2020 г.
Опубликована в печати:	1 июн. 2020 г.
Опубликована online:	24 июл. 2020 г.

Web of science:	WOS:000551935700013
Scopus:	2-s2.0-85088399474
Chemical Abstracts:	2020:1478960
OpenAlex:	W3044874590

БД	Цитирований
Scopus	9
OpenAlex	7
Web of science	8