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Сurrent Tectonic Activity of the Kandalaksha Graben According to a Set of Data. Pp. 21–29.

Версия для печати

Section: Geosciences

UDC

551.64

Authors

Kutinov Yury Grigoryevich, Northern (Arctic) Federal University named after M.V. Lomonosov; Institute of Ecological Problems of the North, Ural Branch of the Russian Academy of Sciences (Arkhangelsk, Russia)

Chistova Zinaida Borisovna, Institute of Ecological Problems of the North, Ural Branch of the Russian Academy of Sciences (Arkhangelsk, Russia)

Gofarov Mikhail Yuryevich, Institute of Ecological Problems of the North, Ural Branch of the Russian Academy of Sciences (Arkhangelsk, Russia)

Mineev Aleksandr Leonidovich, Postgraduate Student, Institute of Ecological Problems of the North, Ural Branch of the Russian Academy of Sciences (Arkhangelsk, Russia)

Abstract

Using remote sensing data, we studied the cloud cover above the Kandalaksha graben and the adjacent territories. The Kandalaksha graben turned out to have practically no cloud cover on the faults limiting the structure during summer, which indicates increased deep degassing. Groundtruth observations indicate deep degassing, changes in the structure of pressure field and induced magnetotelluric currents along the Kandalaksha graben.

Keywords

north of the East European Craton, Kandalaksha graben, remote sensing of the Earth, deep degassing, induced magnetotelluric currents, cloudiness.

The full-text version of the article can be requested through the university’s library.

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