Evolution of sedimentation on the continental slope of the Kronotskii Peninsula (Eastern Kamchatka) over the last 20 ka

Different genetic types of marine sediments that were deposited on the continental slope of the Kronotskii Peninsula with the rate of several tens of centimeters per thousand years during the last 20 ka have been investigated. It is established that their lithological, mineral, and chemical composit...

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Bibliographic Details
Published in:Lithology and Mineral Resources
Main Authors: Levitan, M. A., Kuzmina, T. G., Luksha, V. L., Roshchina, I. A., Syromyatnikov, K. V., Max, L., Nürnberg, Dirk, Riethdorf, Jan-Rainer
Format: Article in Journal/Newspaper
Language:English
Published: Springer 2015
Subjects:
Kamchatka
Online Access:https://oceanrep.geomar.de/id/eprint/29296/
https://oceanrep.geomar.de/id/eprint/29296/1/Levitan.pdf
https://doi.org/10.1134/S0024490215040045
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Summary:Different genetic types of marine sediments that were deposited on the continental slope of the Kronotskii Peninsula with the rate of several tens of centimeters per thousand years during the last 20 ka have been investigated. It is established that their lithological, mineral, and chemical compositions were determined by climate changes.

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