Composition of Eocene claystones of ODP Hole 105-647A ...

Authigenic carbonates were recovered in lower to middle Eocene claystones at Ocean Drilling Program Site 647 in the Labrador Sea. Detailed chemical, petrographic, and X-ray investigations reveal that these diagenetic carbonates have a complex mineralogical composition. At least five different carbon...

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Main Authors: Bohrmann, Gerhard, Thiede, Jörn
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 1989
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.745212
https://doi.pangaea.de/10.1594/PANGAEA.745212
id ftdatacite:10.1594/pangaea.745212
record_format openpolar
spelling ftdatacite:10.1594/pangaea.745212 2024-09-30T14:38:11+00:00 Composition of Eocene claystones of ODP Hole 105-647A ... Bohrmann, Gerhard Thiede, Jörn 1989 application/zip https://dx.doi.org/10.1594/pangaea.745212 https://doi.pangaea.de/10.1594/PANGAEA.745212 en eng PANGAEA https://dx.doi.org/10.2973/odp.proc.sr.105.174.1989 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Drilling/drill rig Leg105 Joides Resolution Ocean Drilling Program ODP Collection Supplementary Publication Series of Datasets article 1989 ftdatacite https://doi.org/10.1594/pangaea.74521210.2973/odp.proc.sr.105.174.1989 2024-09-02T08:36:09Z Authigenic carbonates were recovered in lower to middle Eocene claystones at Ocean Drilling Program Site 647 in the Labrador Sea. Detailed chemical, petrographic, and X-ray investigations reveal that these diagenetic carbonates have a complex mineralogical composition. At least five different carbonate phases are identified: calcium-rich rhodochrosite, rhodochrosite, manganosiderite, siderite, and calcite. Manganese carbonates are the dominant carbonate phases formed throughout the section. Textural analyses show two major generations of carbonate formation. Early cementation of micritic carbonate in burrow structures was followed by carbonate cementation forming microsparry to sparry crystals.At approximately 620 meters below seafloor (mbsf), three concretions of iron carbonates occur, which indicates a special pore-water chemistry. Thin section analyses from this level show (1) several generations of diagenetic carbonates, (2) widespread secondary cavity formation in burrow structures, and (3) various ... : Supplement to: Bohrmann, Gerhard; Thiede, Jörn (1989): Diagenesis in Eocene claystones, ODP Site 647, Labrador Sea: formation of complex authigenic carbonates, smectites, and apatite. 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, 137-154 ... Article in Journal/Newspaper Labrador Sea DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Drilling/drill rig
Leg105
Joides Resolution
Ocean Drilling Program ODP
spellingShingle Drilling/drill rig
Leg105
Joides Resolution
Ocean Drilling Program ODP
Bohrmann, Gerhard
Thiede, Jörn
Composition of Eocene claystones of ODP Hole 105-647A ...
topic_facet Drilling/drill rig
Leg105
Joides Resolution
Ocean Drilling Program ODP
description Authigenic carbonates were recovered in lower to middle Eocene claystones at Ocean Drilling Program Site 647 in the Labrador Sea. Detailed chemical, petrographic, and X-ray investigations reveal that these diagenetic carbonates have a complex mineralogical composition. At least five different carbonate phases are identified: calcium-rich rhodochrosite, rhodochrosite, manganosiderite, siderite, and calcite. Manganese carbonates are the dominant carbonate phases formed throughout the section. Textural analyses show two major generations of carbonate formation. Early cementation of micritic carbonate in burrow structures was followed by carbonate cementation forming microsparry to sparry crystals.At approximately 620 meters below seafloor (mbsf), three concretions of iron carbonates occur, which indicates a special pore-water chemistry. Thin section analyses from this level show (1) several generations of diagenetic carbonates, (2) widespread secondary cavity formation in burrow structures, and (3) various ... : Supplement to: Bohrmann, Gerhard; Thiede, Jörn (1989): Diagenesis in Eocene claystones, ODP Site 647, Labrador Sea: formation of complex authigenic carbonates, smectites, and apatite. 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, 137-154 ...
format Article in Journal/Newspaper
author Bohrmann, Gerhard
Thiede, Jörn
author_facet Bohrmann, Gerhard
Thiede, Jörn
author_sort Bohrmann, Gerhard
title Composition of Eocene claystones of ODP Hole 105-647A ...
title_short Composition of Eocene claystones of ODP Hole 105-647A ...
title_full Composition of Eocene claystones of ODP Hole 105-647A ...
title_fullStr Composition of Eocene claystones of ODP Hole 105-647A ...
title_full_unstemmed Composition of Eocene claystones of ODP Hole 105-647A ...
title_sort composition of eocene claystones of odp hole 105-647a ...
publisher PANGAEA
publishDate 1989
url https://dx.doi.org/10.1594/pangaea.745212
https://doi.pangaea.de/10.1594/PANGAEA.745212
genre Labrador Sea
genre_facet Labrador Sea
op_relation https://dx.doi.org/10.2973/odp.proc.sr.105.174.1989
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.74521210.2973/odp.proc.sr.105.174.1989
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