Paleoseismic Fault Trenches as Unique Archives of the White Sea Holocene History

被引:0
作者
Zaretskaya, N. E. [1 ,2 ]
Ludikova, A. V. [4 ]
Shvarev, S. V. [1 ,3 ]
Kuznetsov, D. D. [4 ]
Kutenkov, S. A. [5 ]
机构
[1] Russian Acad Sci, Inst Geog, Moscow, Russia
[2] Russian Acad Sci, Geol Inst, Moscow, Russia
[3] Russian Acad Sci, Schmidt Inst Phys Earth, Moscow, Russia
[4] Russian Acad Sci, Inst Limnol, St Petersburg, Russia
[5] Russian Acad Sci, Inst Biol, Karelian Res Ctr, Petrozavodsk, Russia
基金
俄罗斯科学基金会;
关键词
White Sea; Holocene; differentiated movements; age; bivalves; diatom analysis; glacioisostatic uplift; SITES;
D O I
10.1134/S1028334X22601249
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
We studied sedimentary archives on the Karelian coast of the White Sea (area of the White Sea Biological Station, Moscow State University) from various objects-filling of the paleoseismic fault trench, marine terraces, and buried shell lenses-to obtain new data on the relative sea level dynamics in the Holocene in the areas where block tectonic movements took place. The specific features of the formation of subfossil malacofauna taphocenoses in Kandalaksha Gulf, changes in the sedimentation environment under the conditions of uplifting coast, and traces of strong seismicity in the late glacial and postglacial periods are also revealed.
引用
收藏
页码:S61 / S68
页数:8
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