Sedimentary facies, clay mineralogy and geochemistry of the Paleogene sediments of ODP Site 105-647 ...
Claystones immediately overlying the early Eocene age ocean-floor basalt, cored at Ocean Drilling Program (ODP) Site 647, underwent hydrothermal and thermal alterations originating from the basalt, which resulted in changes in both the mineralogical and chemical composition of the sediments. Chlorit...
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1989
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Online Access: | https://dx.doi.org/10.1594/pangaea.745194 https://doi.pangaea.de/10.1594/PANGAEA.745194 |
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ftdatacite:10.1594/pangaea.745194 2024-09-30T14:38:12+00:00 Sedimentary facies, clay mineralogy and geochemistry of the Paleogene sediments of ODP Site 105-647 ... Nielsen, Ole Bjorslev Cremer, Michel Stein, Ruediger Thiébault, Francois Zimmerman, Herman 1989 application/zip https://dx.doi.org/10.1594/pangaea.745194 https://doi.pangaea.de/10.1594/PANGAEA.745194 en eng PANGAEA https://dx.doi.org/10.2973/odp.proc.sr.105.116.1989 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Composite Core Leg105 Joides Resolution Ocean Drilling Program ODP Collection Supplementary Publication Series of Datasets article 1989 ftdatacite https://doi.org/10.1594/pangaea.74519410.2973/odp.proc.sr.105.116.1989 2024-09-02T08:36:09Z Claystones immediately overlying the early Eocene age ocean-floor basalt, cored at Ocean Drilling Program (ODP) Site 647, underwent hydrothermal and thermal alterations originating from the basalt, which resulted in changes in both the mineralogical and chemical composition of the sediments. Chlorites and higher magnesium and iron concentrations were found in the lowermost sediment sequence. Upcore, changes in the bulk chemical composition of the sediments become smaller, when compensated for variations in the carbonate content originating from biogenic and authigenic components. Chlorite disappears upcore, but still only part of the swelling clay minerals have survived the thermal influence. Thirty meters above the basalt, the clay mineralogy and chemical composition become uniform throughout the Paleogene section. Iron-rich smectites (i.e., nontronitic types), totally dominate the clay mineral assemblage. Biogenic components, responsible for the dominant part of the calcite and cristobalite contents, vary ... : Supplement to: Nielsen, Ole Bjorslev; Cremer, Michel; Stein, Ruediger; Thiébault, Francois; Zimmerman, Herman (1989): Analysis of sedimentary facies, clay mineralogy, and geochemistry of the Paleogene sediments of Site 647, Labrador Sea. In: Srivastava, SP; Arthur, M; Clement, B; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 105, 101-110 ... Article in Journal/Newspaper Labrador Sea DataCite Zimmerman ENVELOPE(167.167,167.167,-73.300,-73.300) Ciencias Marinas 38 1B 263 286 |
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Open Polar |
collection |
DataCite |
op_collection_id |
ftdatacite |
language |
English |
topic |
Composite Core Leg105 Joides Resolution Ocean Drilling Program ODP |
spellingShingle |
Composite Core Leg105 Joides Resolution Ocean Drilling Program ODP Nielsen, Ole Bjorslev Cremer, Michel Stein, Ruediger Thiébault, Francois Zimmerman, Herman Sedimentary facies, clay mineralogy and geochemistry of the Paleogene sediments of ODP Site 105-647 ... |
topic_facet |
Composite Core Leg105 Joides Resolution Ocean Drilling Program ODP |
description |
Claystones immediately overlying the early Eocene age ocean-floor basalt, cored at Ocean Drilling Program (ODP) Site 647, underwent hydrothermal and thermal alterations originating from the basalt, which resulted in changes in both the mineralogical and chemical composition of the sediments. Chlorites and higher magnesium and iron concentrations were found in the lowermost sediment sequence. Upcore, changes in the bulk chemical composition of the sediments become smaller, when compensated for variations in the carbonate content originating from biogenic and authigenic components. Chlorite disappears upcore, but still only part of the swelling clay minerals have survived the thermal influence. Thirty meters above the basalt, the clay mineralogy and chemical composition become uniform throughout the Paleogene section. Iron-rich smectites (i.e., nontronitic types), totally dominate the clay mineral assemblage. Biogenic components, responsible for the dominant part of the calcite and cristobalite contents, vary ... : Supplement to: Nielsen, Ole Bjorslev; Cremer, Michel; Stein, Ruediger; Thiébault, Francois; Zimmerman, Herman (1989): Analysis of sedimentary facies, clay mineralogy, and geochemistry of the Paleogene sediments of Site 647, Labrador Sea. In: Srivastava, SP; Arthur, M; Clement, B; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 105, 101-110 ... |
format |
Article in Journal/Newspaper |
author |
Nielsen, Ole Bjorslev Cremer, Michel Stein, Ruediger Thiébault, Francois Zimmerman, Herman |
author_facet |
Nielsen, Ole Bjorslev Cremer, Michel Stein, Ruediger Thiébault, Francois Zimmerman, Herman |
author_sort |
Nielsen, Ole Bjorslev |
title |
Sedimentary facies, clay mineralogy and geochemistry of the Paleogene sediments of ODP Site 105-647 ... |
title_short |
Sedimentary facies, clay mineralogy and geochemistry of the Paleogene sediments of ODP Site 105-647 ... |
title_full |
Sedimentary facies, clay mineralogy and geochemistry of the Paleogene sediments of ODP Site 105-647 ... |
title_fullStr |
Sedimentary facies, clay mineralogy and geochemistry of the Paleogene sediments of ODP Site 105-647 ... |
title_full_unstemmed |
Sedimentary facies, clay mineralogy and geochemistry of the Paleogene sediments of ODP Site 105-647 ... |
title_sort |
sedimentary facies, clay mineralogy and geochemistry of the paleogene sediments of odp site 105-647 ... |
publisher |
PANGAEA |
publishDate |
1989 |
url |
https://dx.doi.org/10.1594/pangaea.745194 https://doi.pangaea.de/10.1594/PANGAEA.745194 |
long_lat |
ENVELOPE(167.167,167.167,-73.300,-73.300) |
geographic |
Zimmerman |
geographic_facet |
Zimmerman |
genre |
Labrador Sea |
genre_facet |
Labrador Sea |
op_relation |
https://dx.doi.org/10.2973/odp.proc.sr.105.116.1989 |
op_rights |
Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 |
op_doi |
https://doi.org/10.1594/pangaea.74519410.2973/odp.proc.sr.105.116.1989 |
container_title |
Ciencias Marinas |
container_volume |
38 |
container_issue |
1B |
container_start_page |
263 |
op_container_end_page |
286 |
_version_ |
1811640901257134080 |