The white sea level change and glacioisostatic land uplift during the Holocene near the Settlement of Kuzema, North Karelia Region-Reference-Cited by-同舟云学术

The white sea level change and glacioisostatic land uplift during the Holocene near the Settlement of Kuzema, North Karelia Region

Published:2012-01 Issue:1 Volume:442 Page:139-143
ISSN:1028-334X
Container-title:Doklady Earth Sciences
language:en
Short-container-title:Dokl. Earth Sc.

Author:

Kolka V. V.,Korsakova O. P.,Shelekhova T. S.,Lavrova N. B.,Arslanov Kh. A.

Publisher

Pleiades Publishing Ltd

Subject

General Earth and Planetary Sciences,Earth and Planetary Sciences (miscellaneous)

Link

http://link.springer.com/content/pdf/10.1134/S1028334X12010151.pdf

Reference4 articles.

1. I. Ekman and V. Iljin, in Eastern Fennoscandian Younger Dryas and Moraines (Geol. Surv. Finland, Helsinki, 1991), pp. 73–99.

2. V. V. Kolka, V. Ya. Evzerov, J. J. Moller, and G. D. Corner, in New Data on Geology and Useful Mineral Resources in the Kola Peninsular (Izd-vo KSC RAS, Apatity, 2005), pp. 15–25 [in Russian].

3. J. Donner, M. Eronen, and H. Jungner, Norsk Geograf. Tidsskrift. 31, 103–128 (1977).

4. A. D. Lukashov, Paleoseismotectonics in the Northern Part of Lake Onega (Zaonezhskij Peninsula, Russian Karelia) (Geol. Surv. Finland; Nuclear Waste Disposal Research, Helsinki, 1995).

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