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Sedimentation rate in Cheko Lake (Evenkia, Siberia): new evidence on the problem of the 1908 Tunguska Event
D. Y. Rogozin, A. V. Darin, I. A. Kalugin et al., 2017. Doklady Earth Sciences 476(2), 1226–1228.
137Cs and 210Pb activity profiles and counted varves in a Cheko core indicate the lake is much older than 1908 and so cannot be a crater of the event.
What it's used for here
The sediment-dating case against the crater reading.
Our copy
Research copy, for editors and curators. The work is the publisher's, so readers are sent to it. We keep this copy so the citation can be checked if the page changes or goes.
doi.org · fetched 27 Oct 2026
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Cited by on this site 6 records
The 1908 Tunguska event
MYSThe mystery article
Cite it
Rogozin, D. Y., Darin, A. V., Kalugin, I. A., Melgunov, M. S., Meydus, A. V., & Degermendzhi, A. G. (2017). Sedimentation rate in Cheko Lake (Evenkia, Siberia): new evidence on the problem of the 1908 Tunguska Event. Doklady Earth Sciences 476(2), 1226–1228. https://doi.org/10.1134/S1028334X17100269
@article{rogozin2017cheko,
author = {Rogozin, D. Y. and Darin, A. V. and Kalugin, I. A. and Melgunov, M. S. and Meydus, A. V. and Degermendzhi, A. G.},
title = {Sedimentation rate in Cheko Lake (Evenkia, Siberia): new evidence on the problem of the 1908 Tunguska Event},
journal = {Doklady Earth Sciences 476(2), 1226–1228},
year = {2017},
doi = {10.1134/S1028334X17100269},
url = {https://doi.org/10.1134/S1028334X17100269}
}TY - JOUR TI - Sedimentation rate in Cheko Lake (Evenkia, Siberia): new evidence on the problem of the 1908 Tunguska Event AU - Rogozin, D. Y. AU - Darin, A. V. AU - Kalugin, I. A. AU - Melgunov, M. S. AU - Meydus, A. V. AU - Degermendzhi, A. G. PY - 2017 JO - Doklady Earth Sciences 476(2), 1226–1228 DO - 10.1134/S1028334X17100269 UR - https://doi.org/10.1134/S1028334X17100269 ER -
Rogozin, D. Y. et al.. “Sedimentation rate in Cheko Lake (Evenkia, Siberia): new evidence on the problem of the 1908 Tunguska Event.” Doklady Earth Sciences 476(2), 1226–1228 (2017). https://doi.org/10.1134/S1028334X17100269.