Composition of bottom sediments from the Guinea Basin

Geomorphology of the Guinea Basin is described along with sediments from cores collected on the abyssal plain, within the abyssal hill zone, and in the eastern part of the Chain Fracture Zone. Stratigraphic differentiation of deep-sea sediments was based on diatom analysis, geochemical and lithologi...

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Bibliographic Details
Main Authors: Lavrov, Vadim M, Savel'yeva, K P
Format: Dataset
Language:English
Published: PANGAEA 1971
Subjects:
Archive of Ocean Data
ARCOD
Grab
Gulf of Guinea
Mikhail Lomonosov
ML10
ML10_827
ML10_829
ML10_837
ML10_846
ML10_847
ML10_848
ML10_850
MULT
Multiple investigations
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.753701
https://doi.org/10.1594/PANGAEA.753701
id ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.753701
record_format openpolar
spelling ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.753701 2023-05-15T17:12:45+02:00 Composition of bottom sediments from the Guinea Basin Lavrov, Vadim M Savel'yeva, K P MEDIAN LATITUDE: 1.303562 * MEDIAN LONGITUDE: -4.098309 * SOUTH-BOUND LATITUDE: -1.001000 * WEST-BOUND LONGITUDE: -11.016000 * NORTH-BOUND LATITUDE: 4.333300 * EAST-BOUND LONGITUDE: -1.636000 1971-11-16 application/zip, 5 datasets https://doi.pangaea.de/10.1594/PANGAEA.753701 https://doi.org/10.1594/PANGAEA.753701 en eng PANGAEA https://doi.pangaea.de/10.1594/PANGAEA.753701 https://doi.org/10.1594/PANGAEA.753701 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess CC-BY Supplement to: Lavrov, Vadim M; Savel'yeva, K P (1971): Deep-water sediments in the Guinea Basin. Oceanology, 11, 551-562 Archive of Ocean Data ARCOD Grab Gulf of Guinea Mikhail Lomonosov ML10 ML10_827 ML10_829 ML10_837 ML10_846 ML10_847 ML10_848 ML10_850 MULT Multiple investigations Dataset 1971 ftpangaea https://doi.org/10.1594/PANGAEA.753701 2023-01-20T07:31:58Z Geomorphology of the Guinea Basin is described along with sediments from cores collected on the abyssal plain, within the abyssal hill zone, and in the eastern part of the Chain Fracture Zone. Stratigraphic differentiation of deep-sea sediments was based on diatom analysis, geochemical and lithological data. Holocene and Pleistocene were identified by these criteria. The lower boundary of Holocene is was found from a marked decrease in CaCO3 concentration and total diatom count. Mineral and chemical compositions are given for coarse silt fraction of various Late Pleistocene sediments. It is shown that this facial complex is determined by tectonic position of the Guinea Basin. Dataset Mikhail Lomonosov PANGAEA - Data Publisher for Earth & Environmental Science ENVELOPE(-11.016000,-1.636000,4.333300,-1.001000)
institution Open Polar
collection PANGAEA - Data Publisher for Earth & Environmental Science
op_collection_id ftpangaea
language English
topic Archive of Ocean Data
ARCOD
Grab
Gulf of Guinea
Mikhail Lomonosov
ML10
ML10_827
ML10_829
ML10_837
ML10_846
ML10_847
ML10_848
ML10_850
MULT
Multiple investigations
spellingShingle Archive of Ocean Data
ARCOD
Grab
Gulf of Guinea
Mikhail Lomonosov
ML10
ML10_827
ML10_829
ML10_837
ML10_846
ML10_847
ML10_848
ML10_850
MULT
Multiple investigations
Lavrov, Vadim M
Savel'yeva, K P
Composition of bottom sediments from the Guinea Basin
topic_facet Archive of Ocean Data
ARCOD
Grab
Gulf of Guinea
Mikhail Lomonosov
ML10
ML10_827
ML10_829
ML10_837
ML10_846
ML10_847
ML10_848
ML10_850
MULT
Multiple investigations
description Geomorphology of the Guinea Basin is described along with sediments from cores collected on the abyssal plain, within the abyssal hill zone, and in the eastern part of the Chain Fracture Zone. Stratigraphic differentiation of deep-sea sediments was based on diatom analysis, geochemical and lithological data. Holocene and Pleistocene were identified by these criteria. The lower boundary of Holocene is was found from a marked decrease in CaCO3 concentration and total diatom count. Mineral and chemical compositions are given for coarse silt fraction of various Late Pleistocene sediments. It is shown that this facial complex is determined by tectonic position of the Guinea Basin.
format Dataset
author Lavrov, Vadim M
Savel'yeva, K P
author_facet Lavrov, Vadim M
Savel'yeva, K P
author_sort Lavrov, Vadim M
title Composition of bottom sediments from the Guinea Basin
title_short Composition of bottom sediments from the Guinea Basin
title_full Composition of bottom sediments from the Guinea Basin
title_fullStr Composition of bottom sediments from the Guinea Basin
title_full_unstemmed Composition of bottom sediments from the Guinea Basin
title_sort composition of bottom sediments from the guinea basin
publisher PANGAEA
publishDate 1971
url https://doi.pangaea.de/10.1594/PANGAEA.753701
https://doi.org/10.1594/PANGAEA.753701
op_coverage MEDIAN LATITUDE: 1.303562 * MEDIAN LONGITUDE: -4.098309 * SOUTH-BOUND LATITUDE: -1.001000 * WEST-BOUND LONGITUDE: -11.016000 * NORTH-BOUND LATITUDE: 4.333300 * EAST-BOUND LONGITUDE: -1.636000
long_lat ENVELOPE(-11.016000,-1.636000,4.333300,-1.001000)
genre Mikhail Lomonosov
genre_facet Mikhail Lomonosov
op_source Supplement to: Lavrov, Vadim M; Savel'yeva, K P (1971): Deep-water sediments in the Guinea Basin. Oceanology, 11, 551-562
op_relation https://doi.pangaea.de/10.1594/PANGAEA.753701
https://doi.org/10.1594/PANGAEA.753701
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.753701
_version_ 1766069590732832768

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