scholarly journals GEOECOLOGICAL ASPECT IN THE ACCUMULATION OF WATER AND BOTTOM SEDIMENTS AND HYDROBIONTS IN THE RIVER BASIN AND THE MIDDLE COURSE OF THE PECHORA RIVER

Author(s):  
V.V. Mazur ◽  
G.N. Dorovskikh
2012 ◽  
Vol 94 (3) ◽  
pp. 525-544 ◽  
Author(s):  
Harieth Hellar-Kihampa ◽  
Sanja Potgieter-Vermaak ◽  
Katleen Van Meel ◽  
Giuliana Gatto Rotondo ◽  
Michael Kishimba ◽  
...  

2012 ◽  
Vol 185 (7) ◽  
pp. 5993-6002 ◽  
Author(s):  
Leticia Peluso ◽  
Gustavo Bulus Rossini ◽  
Alfredo Salibián ◽  
Alicia Ronco

2018 ◽  
Vol 316 (2) ◽  
pp. 805-818 ◽  
Author(s):  
D. I. T. Favaro ◽  
F. R. Rocha ◽  
M. Angelini ◽  
H. R. A Henriques ◽  
J. S. Soares ◽  
...  

2019 ◽  
Vol 485 (2) ◽  
pp. 207-211
Author(s):  
A. V. Maslov ◽  
N. V. Politova ◽  
V. P. Shevchenko ◽  
N. V. Kozina ◽  
A. N. Novigatsk ◽  
...  

The Co, Hf, Ce, Cr, Th, and REE systematics are analyzed for modern sediments collected by a bottom grab during the 67th and 68th cruises of R/V “Akademik Mstislav Keldysh” and samples taken in the Barents Sea bays and inlets. Our results indicate that most modern bottom sediments are composed of fine silicoclastic material enhanced with a suspended matter of the North Cape current, which erodes the western coast of Scandinavia, and due to bottom erosion of some marine areas, as well as erosion of rock complexes of the Kola Peninsula, Novaya Zemlya, and Franz Josef Land (local provenances). Material from Spitsbergen also probably played a certain role. In the southern part of the Barents Sea, clastic material is supplied by the Pechora River.


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