(Table 1) Types of White Sea surface layer bottom sediments and concentration of heavy minerals in 0.1-0.05 mm grain size fraction

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 composi...

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Bibliographic Details
Main Author: Gusakova, A I
Format: Dataset
Language:English
Published: PANGAEA 2013
Subjects:
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.818116
https://doi.org/10.1594/PANGAEA.818116
id ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.818116
record_format openpolar
spelling ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.818116 2023-05-15T18:43:45+02:00 (Table 1) Types of White Sea surface layer bottom sediments and concentration of heavy minerals in 0.1-0.05 mm grain size fraction Gusakova, A I 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 2013-08-16 text/tab-separated-values, 261 data points https://doi.pangaea.de/10.1594/PANGAEA.818116 https://doi.org/10.1594/PANGAEA.818116 en eng PANGAEA 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 https://doi.pangaea.de/10.1594/PANGAEA.818116 https://doi.org/10.1594/PANGAEA.818116 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess CC-BY P.P. Shirshov Institute of Oceanology, Russian Academy of Sciences, Moscow Archive of Ocean Data ARCOD Depth bottom/max sediment/rock top/min Ekolog-2006-111 Ekolog-2006-118 Ekolog-2006-19 Ekolog-2006-52 Ekolog-2006-54 Ekolog-2008-32 Ekolog-2008-33 Ekolog-2009-17 Ekolog-2009-18 Ekolog-2009-38 Ekolog-2009-47 Ekolog-2009-48 Ekolog-2010-02 Ekolog-2010-16 Ekolog-2010-17 Ekolog-2010-23 Ekolog-2010-48 Ekolog-2011-10 Ekolog-2011-11 Elevation of event Event label Heavy minerals JUDAY Juday net Latitude of event Lithological description Longitude of event MULT Multiple investigations Professor Shtokman PSh49 PSh49-4684 PSh49-4685 PSh49-4687 PSh49-4688 PSh49-4691 PSh49-4692 PSh49-4693 PSh49-4694 PSh49-4697 PSh49-4699 PSh49-4700 Dataset 2013 ftpangaea https://doi.org/10.1594/PANGAEA.818116 https://doi.org/10.1134/S0001437013020045 2023-01-20T09:01:30Z 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. Dataset White Sea PANGAEA - Data Publisher for Earth & Environmental Science White Sea ENVELOPE(33.642667,40.671167,66.655833,64.588167)
institution Open Polar
collection PANGAEA - Data Publisher for Earth & Environmental Science
op_collection_id ftpangaea
language English
topic Archive of Ocean Data
ARCOD
Depth
bottom/max
sediment/rock
top/min
Ekolog-2006-111
Ekolog-2006-118
Ekolog-2006-19
Ekolog-2006-52
Ekolog-2006-54
Ekolog-2008-32
Ekolog-2008-33
Ekolog-2009-17
Ekolog-2009-18
Ekolog-2009-38
Ekolog-2009-47
Ekolog-2009-48
Ekolog-2010-02
Ekolog-2010-16
Ekolog-2010-17
Ekolog-2010-23
Ekolog-2010-48
Ekolog-2011-10
Ekolog-2011-11
Elevation of event
Event label
Heavy minerals
JUDAY
Juday net
Latitude of event
Lithological description
Longitude of event
MULT
Multiple investigations
Professor Shtokman
PSh49
PSh49-4684
PSh49-4685
PSh49-4687
PSh49-4688
PSh49-4691
PSh49-4692
PSh49-4693
PSh49-4694
PSh49-4697
PSh49-4699
PSh49-4700
spellingShingle Archive of Ocean Data
ARCOD
Depth
bottom/max
sediment/rock
top/min
Ekolog-2006-111
Ekolog-2006-118
Ekolog-2006-19
Ekolog-2006-52
Ekolog-2006-54
Ekolog-2008-32
Ekolog-2008-33
Ekolog-2009-17
Ekolog-2009-18
Ekolog-2009-38
Ekolog-2009-47
Ekolog-2009-48
Ekolog-2010-02
Ekolog-2010-16
Ekolog-2010-17
Ekolog-2010-23
Ekolog-2010-48
Ekolog-2011-10
Ekolog-2011-11
Elevation of event
Event label
Heavy minerals
JUDAY
Juday net
Latitude of event
Lithological description
Longitude of event
MULT
Multiple investigations
Professor Shtokman
PSh49
PSh49-4684
PSh49-4685
PSh49-4687
PSh49-4688
PSh49-4691
PSh49-4692
PSh49-4693
PSh49-4694
PSh49-4697
PSh49-4699
PSh49-4700
Gusakova, A I
(Table 1) Types of White Sea surface layer bottom sediments and concentration of heavy minerals in 0.1-0.05 mm grain size fraction
topic_facet Archive of Ocean Data
ARCOD
Depth
bottom/max
sediment/rock
top/min
Ekolog-2006-111
Ekolog-2006-118
Ekolog-2006-19
Ekolog-2006-52
Ekolog-2006-54
Ekolog-2008-32
Ekolog-2008-33
Ekolog-2009-17
Ekolog-2009-18
Ekolog-2009-38
Ekolog-2009-47
Ekolog-2009-48
Ekolog-2010-02
Ekolog-2010-16
Ekolog-2010-17
Ekolog-2010-23
Ekolog-2010-48
Ekolog-2011-10
Ekolog-2011-11
Elevation of event
Event label
Heavy minerals
JUDAY
Juday net
Latitude of event
Lithological description
Longitude of event
MULT
Multiple investigations
Professor Shtokman
PSh49
PSh49-4684
PSh49-4685
PSh49-4687
PSh49-4688
PSh49-4691
PSh49-4692
PSh49-4693
PSh49-4694
PSh49-4697
PSh49-4699
PSh49-4700
description 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.
format Dataset
author Gusakova, A I
author_facet Gusakova, A I
author_sort Gusakova, A I
title (Table 1) Types of White Sea surface layer bottom sediments and concentration of heavy minerals in 0.1-0.05 mm grain size fraction
title_short (Table 1) Types of White Sea surface layer bottom sediments and concentration of heavy minerals in 0.1-0.05 mm grain size fraction
title_full (Table 1) Types of White Sea surface layer bottom sediments and concentration of heavy minerals in 0.1-0.05 mm grain size fraction
title_fullStr (Table 1) Types of White Sea surface layer bottom sediments and concentration of heavy minerals in 0.1-0.05 mm grain size fraction
title_full_unstemmed (Table 1) Types of White Sea surface layer bottom sediments and concentration of heavy minerals in 0.1-0.05 mm grain size fraction
title_sort (table 1) types of white sea surface layer bottom sediments and concentration of heavy minerals in 0.1-0.05 mm grain size fraction
publisher PANGAEA
publishDate 2013
url https://doi.pangaea.de/10.1594/PANGAEA.818116
https://doi.org/10.1594/PANGAEA.818116
op_coverage 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
long_lat ENVELOPE(33.642667,40.671167,66.655833,64.588167)
geographic White Sea
geographic_facet White Sea
genre White Sea
genre_facet White Sea
op_source P.P. Shirshov Institute of Oceanology, Russian Academy of Sciences, Moscow
op_relation 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
https://doi.pangaea.de/10.1594/PANGAEA.818116
https://doi.org/10.1594/PANGAEA.818116
op_rights CC-BY-3.0: Creative Commons Attribution 3.0 Unported
Access constraints: unrestricted
info:eu-repo/semantics/openAccess
op_rightsnorm CC-BY
op_doi https://doi.org/10.1594/PANGAEA.818116
https://doi.org/10.1134/S0001437013020045
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