scholarly journals NATURAL PHENOMENA OF ENDOGENIC ORIGIN IN THE ARCTIC BASIN

Author(s):  
A.A. Petrova ◽  
◽  
O.V. Latysheva ◽  
Yu.A. Kopytenko ◽  
◽  
...  

The results of the study of the influence of the deep factor on the process of melting of the ice cover of the Arctic Ocean and the formation of dangerous natural phenomena are presented. The peculiarities of the structure of the earth’s crust contributing to the ice destruction are visualized based on the interpretation of anomalies of the magnetic field and gravity. Density and magnetic sections of the bottom structures are constructed taking into account seismic and seismological data. Two-dimensional density calculations of the Arctic crust density have been performed to detect fluid-saturated layers. Analysis of satellite observations of ice condition together with interpretation of gravity and magnetic data made it possible to identify natural phenomena of endogenous origin, caused by influence of thermo fluid flows of the earth’s crust. The study of annual and seasonal changes in the thickness of multiyear ice over the period 2007–2020 has shown that a decisive role in the thawing process is played by fluid-supplying channels of deep-seated fault zones. The role of an endogenous factor in the destruction of ice of different ages and in the emergence of dangerous phenomena in the areas of hydrate development has been revealed. This makes it possible to predict the localization of zones of variability in the thickness of multiyear ice, the nature of the destruction of its edges and reduce the risks of navigation.

Geotectonics ◽  
2007 ◽  
Vol 41 (4) ◽  
pp. 296-305 ◽  
Author(s):  
V. A. Poselov ◽  
V. V. Verba ◽  
S. M. Zholondz

1978 ◽  
Vol 13 (1-4) ◽  
pp. 339-359 ◽  
Author(s):  
P. Gloersen ◽  
H. J. Zwally ◽  
A. T. C. Chang ◽  
D. K. Hall ◽  
W. J. Campbell ◽  
...  

2020 ◽  
Vol 19 (4) ◽  
pp. 517-526
Author(s):  
Pham Nam Hung ◽  
Cao Dinh Trong ◽  
Le Van Dung ◽  
Thai Anh Tuan ◽  
Mai Xuan Bach ◽  
...  

This paper presents the structural characteristics of the Earth’s crust in Thua Thien-Hue province and adjacent area based on interpretation of gravity and magnetic data in combination. Research results have shown that: The depth of crystalline basement varies complicatedly, in the range of 0–11 km. The depth of Conrad surface increases from Northeast (12 km) to Southwest (18 km) and the depth of Moho surface is 23–34 km; The density of sedimentary layer changes from 2.61 g/cm3 to 2.65 g/cm3. Meanwhile, the density of granitic layer is in the range of 2.68–2.73 g/cm3. The basaltic layer has the density value of 2.88–2.93 g/cm3 and the average density of lower layer of the Earth’s crust is about 3.30 g/cm3; The depth of second-order faults, Red River and A Luoi - Rao Quan, is through the Earth’s crust. Meanwhile, the depth of influence of third-order faults, Chay river, Dong Ha - Phu Vang, Vinh Linh, Hue - Son Tra and Tam Ky - Phuoc Son, is within the thickness of the Earth’s crust.


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