naa a22 4500 510765505 CHVBK 20180411083155.0 cr unu---uuuuu 180411e20130301xx s 000 0 eng 10.1134/S0001437013020045 doi (NATIONALLICENCE)springer-10.1134/S0001437013020045 Gusakova A. Shirshov Institute of Oceanology, Russian Academy of Sciences, Moscow, Russia aut Mineral composition of the modern bottom sediments of the White Sea [Elektronische Daten] [A. Gusakova] The mineral composition of the modern bottom sediments were studied in the White Sea. The single terrigenous-mineralogical province is defined; it is characterized by the mineral association of amphibole, epidote, garnet, and pyroxene. Five regions are assigned in the White Sea in accordance with the mineral composition of the surface bottom sediments. We argue that the granite-metamorphic rock complexes of the Baltic Shield are the main source of the modern sediments in the White Sea, while the East European Craton (Russian Platform) plays a secondary role. Pleiades Publishing, Ltd., 2013 Oceanology SP MAIK Nauka/Interperiodica 53/2(2013-03-01), 223-232 0001-4370 53:2<223 2013 53 11491 https://doi.org/10.1134/S0001437013020045 text/html Onlinezugriff via DOI 1 research-article jats NATIONALLICENCE 856 40 https://doi.org/10.1134/S0001437013020045 text/html Onlinezugriff via DOI NATIONALLICENCE 100 1- Gusakova A. Shirshov Institute of Oceanology, Russian Academy of Sciences, Moscow, Russia aut NATIONALLICENCE 773 0- Oceanology SP MAIK Nauka/Interperiodica 53/2(2013-03-01), 223-232 0001-4370 53:2<223 2013 53 11491 Metadata rights reserved Springer special CC-BY-NC licence nationallicence BK010053 XK010053 XK010000 NATIONALLICENCE NATIONALLICENCE NL-springer