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dc.contributor.author Gusakova, A I
dc.coverage.spatial MEDIAN LATITUDE: 65.418715 * MEDIAN LONGITUDE: 37.378933 * SOUTH-BOUND LATITUDE: 64.588167 * WEST-BOUND LONGITUDE: 33.642667 * NORTH-BOUND LATITUDE: 66.655833 * EAST-BOUND LONGITUDE: 40.671167 * MINIMUM DEPTH, sediment/rock: 0.025 m * MAXIMUM DEPTH, sediment/rock: 0.025 m
dc.date.accessioned 2019-11-13T05:45:56Z
dc.date.available 2019-11-13T05:45:56Z
dc.date.issued 2013-08-16
dc.identifier https://doi.pangaea.de/10.1594/PANGAEA.818116
dc.identifier https://doi.org/10.1594/PANGAEA.818116
dc.identifier.citation Gusakova, A I (2013): Mineral composition of the modern bottom sediments of the White Sea. Translated from Okeanologiya, 2013, 53(2), 249-258, Oceanology, 53(2), 223-232, https://doi.org/10.1134/S0001437013020045
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/6580
dc.description.abstract Mineral composition of recent bottom sediments was studied in the White Sea. A single terrigenous-mineralogical province is defined; it is characterized by a mineral association of amphibole, epidote, garnet, and pyroxene. Five regions are assigned in the White Sea in accordance with mineral composition of surface bottom sediments. We argue that granite-metamorphic rock complexes of the Baltic Shield are the main source of recent bottom sediments in the White Sea, while the East European Craton (Russian Platform) plays the secondary role.
dc.format text/tab-separated-values, 261 data points
dc.language.iso en
dc.publisher PANGAEA
dc.relation.isbasedon Gusakova, A I (2013): Mineral composition of the modern bottom sediments of the White Sea. Translated from Okeanologiya, 2013, 53(2), 249-258, Oceanology, 53(2), 223-232, https://doi.org/10.1134/S0001437013020045
dc.rights CC-BY-3.0: Creative Commons Attribution 3.0 Unported
dc.rights Access constraints: unrestricted
dc.source P.P. Shirshov Institute of Oceanology, Russian Academy of Sciences, Moscow
dc.subject Archive of Ocean Data
dc.subject ARCOD
dc.subject DEPTH, sediment/rock
dc.subject Ekolog-2006-111
dc.subject Ekolog-2006-118
dc.subject Ekolog-2006-19
dc.subject Ekolog-2006-52
dc.subject Ekolog-2006-54
dc.subject Ekolog-2008-32
dc.subject Ekolog-2008-33
dc.subject Ekolog-2009-17
dc.subject Ekolog-2009-18
dc.subject Ekolog-2009-38
dc.subject Ekolog-2009-47
dc.subject Ekolog-2009-48
dc.subject Ekolog-2010-02
dc.subject Ekolog-2010-16
dc.subject Ekolog-2010-17
dc.subject Ekolog-2010-23
dc.subject Ekolog-2010-48
dc.subject Ekolog-2011-10
dc.subject Ekolog-2011-11
dc.subject Heavy minerals
dc.subject JUDAY
dc.subject Juday net
dc.subject Lithological description
dc.subject MULT
dc.subject Professor Shtokman
dc.subject PSh49
dc.subject PSh49-4684
dc.subject PSh49-4685
dc.subject PSh49-4687
dc.subject PSh49-4688
dc.subject PSh49-4691
dc.subject PSh49-4692
dc.subject PSh49-4693
dc.subject PSh49-4694
dc.subject PSh49-4697
dc.subject PSh49-4699
dc.subject PSh49-4700
dc.subject PSh49-4701
dc.subject PSh49-4702
dc.subject PSh49-4704
dc.subject PSh49-4706
dc.subject PSh49-4709
dc.subject PSh49-4715
dc.subject PSh49-4716
dc.subject PSh49-4717
dc.subject PSh49-4718
dc.subject PSh49-4719
dc.subject PSh49-4720
dc.subject PSh49-4721
dc.subject PSh49-4723
dc.subject PSh49-4724
dc.subject PSh49-4725
dc.subject PSh49-4726
dc.subject PSh49-4727
dc.subject PSh49-4728
dc.subject PSh49-4729
dc.subject PSh55
dc.subject Psh55-4918
dc.subject PSh55-4930
dc.subject PSh55-4932
dc.subject PSh55-4934
dc.subject Psh55-4941
dc.subject PSh-7125
dc.subject PSh-7134
dc.subject PSh-7137
dc.subject PSh-7141
dc.subject PSh80
dc.subject PSh80-6046
dc.subject PSh80-6050
dc.subject PSh80-6053
dc.subject PSh80-6054
dc.subject PSh80-6060
dc.subject PSh80-6062
dc.subject PSh80-6063
dc.subject PSh80-6067
dc.subject Sediment type
dc.subject Separation with use of heavy liquid
dc.subject White Sea
dc.title Mineral composition of the modern bottom sediments of the White Sea.
dc.title.alternative (Table 1) Types of White Sea surface layer bottom sediments and concentration of heavy minerals in 0.1-0.05 mm grain size fraction
dc.type Dataset


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