Tab. 3: Differentiation of eroded material in the Arctic Russian Seas
Volumes of Holocene (10 000 years) terrigenous sediments and annnal sediment supply in the Laptev Sea were evaluated from average thickness of the Holocene veneer. Volumes of deposits supplied from various sediment sourees and by different proeesses (abrasion of hinterland and island shores, river d...
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ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.759246 2023-05-15T15:03:15+02:00 Tab. 3: Differentiation of eroded material in the Arctic Russian Seas Kosheleva, Vera A Yashin, Dmitry Musatov, Evgeny E MEDIAN LATITUDE: 74.000000 * MEDIAN LONGITUDE: 116.000000 * SOUTH-BOUND LATITUDE: 70.000000 * WEST-BOUND LONGITUDE: 26.000000 * NORTH-BOUND LATITUDE: 77.000000 * EAST-BOUND LONGITUDE: -171.000000 2001-12-06 text/tab-separated-values, 55 data points https://doi.pangaea.de/10.1594/PANGAEA.759246 https://doi.org/10.1594/PANGAEA.759246 en eng PANGAEA https://doi.pangaea.de/10.1594/PANGAEA.759246 https://doi.org/10.1594/PANGAEA.759246 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess CC-BY Supplement to: Kosheleva, Vera A; Yashin, Dmitry; Musatov, Evgeny E (2001): On the volume of terrigenous sedimentation in the Laptev Sea. Polarforschung, 69, 207-210, hdl:10013/epic.29845.d001 Abrasion Barents Barents Sea Chukchi Chukchi Sea East Siberian Sea E-Siberian_Sea Event label Kara Kara Sea LAP Laptev Sea Latitude of event Longitude of event Dataset 2001 ftpangaea https://doi.org/10.1594/PANGAEA.759246 2023-01-20T08:52:07Z Volumes of Holocene (10 000 years) terrigenous sediments and annnal sediment supply in the Laptev Sea were evaluated from average thickness of the Holocene veneer. Volumes of deposits supplied from various sediment sourees and by different proeesses (abrasion of hinterland and island shores, river discharge, eolian input, drifting ice) were diseriminating of deposition in the eoastal zone, at river/sea barrier, and in the shelf basin itself. Accumulation by drifting iee and the role of local sea bottom erosion were also considered. Total amount of sediments transported from the Laptev Sea shelf to Amundsen and Nansen Basins of the Aretie Ocean was compared with other Russian Aretie seas. Dataset Arctic Barents Sea Chukchi Chukchi Sea East Siberian Sea Kara Sea laptev Laptev Sea Nansen Polarforschung PANGAEA - Data Publisher for Earth & Environmental Science Arctic Barents Sea Laptev Sea Kara Sea Chukchi Sea East Siberian Sea ENVELOPE(166.000,166.000,74.000,74.000) ENVELOPE(26.000000,-171.000000,77.000000,70.000000) |
institution |
Open Polar |
collection |
PANGAEA - Data Publisher for Earth & Environmental Science |
op_collection_id |
ftpangaea |
language |
English |
topic |
Abrasion Barents Barents Sea Chukchi Chukchi Sea East Siberian Sea E-Siberian_Sea Event label Kara Kara Sea LAP Laptev Sea Latitude of event Longitude of event |
spellingShingle |
Abrasion Barents Barents Sea Chukchi Chukchi Sea East Siberian Sea E-Siberian_Sea Event label Kara Kara Sea LAP Laptev Sea Latitude of event Longitude of event Kosheleva, Vera A Yashin, Dmitry Musatov, Evgeny E Tab. 3: Differentiation of eroded material in the Arctic Russian Seas |
topic_facet |
Abrasion Barents Barents Sea Chukchi Chukchi Sea East Siberian Sea E-Siberian_Sea Event label Kara Kara Sea LAP Laptev Sea Latitude of event Longitude of event |
description |
Volumes of Holocene (10 000 years) terrigenous sediments and annnal sediment supply in the Laptev Sea were evaluated from average thickness of the Holocene veneer. Volumes of deposits supplied from various sediment sourees and by different proeesses (abrasion of hinterland and island shores, river discharge, eolian input, drifting ice) were diseriminating of deposition in the eoastal zone, at river/sea barrier, and in the shelf basin itself. Accumulation by drifting iee and the role of local sea bottom erosion were also considered. Total amount of sediments transported from the Laptev Sea shelf to Amundsen and Nansen Basins of the Aretie Ocean was compared with other Russian Aretie seas. |
format |
Dataset |
author |
Kosheleva, Vera A Yashin, Dmitry Musatov, Evgeny E |
author_facet |
Kosheleva, Vera A Yashin, Dmitry Musatov, Evgeny E |
author_sort |
Kosheleva, Vera A |
title |
Tab. 3: Differentiation of eroded material in the Arctic Russian Seas |
title_short |
Tab. 3: Differentiation of eroded material in the Arctic Russian Seas |
title_full |
Tab. 3: Differentiation of eroded material in the Arctic Russian Seas |
title_fullStr |
Tab. 3: Differentiation of eroded material in the Arctic Russian Seas |
title_full_unstemmed |
Tab. 3: Differentiation of eroded material in the Arctic Russian Seas |
title_sort |
tab. 3: differentiation of eroded material in the arctic russian seas |
publisher |
PANGAEA |
publishDate |
2001 |
url |
https://doi.pangaea.de/10.1594/PANGAEA.759246 https://doi.org/10.1594/PANGAEA.759246 |
op_coverage |
MEDIAN LATITUDE: 74.000000 * MEDIAN LONGITUDE: 116.000000 * SOUTH-BOUND LATITUDE: 70.000000 * WEST-BOUND LONGITUDE: 26.000000 * NORTH-BOUND LATITUDE: 77.000000 * EAST-BOUND LONGITUDE: -171.000000 |
long_lat |
ENVELOPE(166.000,166.000,74.000,74.000) ENVELOPE(26.000000,-171.000000,77.000000,70.000000) |
geographic |
Arctic Barents Sea Laptev Sea Kara Sea Chukchi Sea East Siberian Sea |
geographic_facet |
Arctic Barents Sea Laptev Sea Kara Sea Chukchi Sea East Siberian Sea |
genre |
Arctic Barents Sea Chukchi Chukchi Sea East Siberian Sea Kara Sea laptev Laptev Sea Nansen Polarforschung |
genre_facet |
Arctic Barents Sea Chukchi Chukchi Sea East Siberian Sea Kara Sea laptev Laptev Sea Nansen Polarforschung |
op_source |
Supplement to: Kosheleva, Vera A; Yashin, Dmitry; Musatov, Evgeny E (2001): On the volume of terrigenous sedimentation in the Laptev Sea. Polarforschung, 69, 207-210, hdl:10013/epic.29845.d001 |
op_relation |
https://doi.pangaea.de/10.1594/PANGAEA.759246 https://doi.org/10.1594/PANGAEA.759246 |
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.759246 |
_version_ |
1766335130396262400 |