Thorium and uranium isotopes in upper Pleistocene sediments of the Baffin Bay ...

Concentrations and activity ratios of uranium and thorium isotopes (234U/238U, 230Th/232Th) were determined at about 5-m intervals through the composite top 22-m sequence of Ocean Drilling Program (ODP) Hole 645 in Baffin Bay and, in the Labrador Sea, at 1-m intervals through the top 11 m of Core 84...

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Main Authors: Causse, Christiane, Vörösmarty, Charles J
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 1989
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.744863
https://doi.pangaea.de/10.1594/PANGAEA.744863
id ftdatacite:10.1594/pangaea.744863
record_format openpolar
spelling ftdatacite:10.1594/pangaea.744863 2024-09-15T17:56:54+00:00 Thorium and uranium isotopes in upper Pleistocene sediments of the Baffin Bay ... Causse, Christiane Vörösmarty, Charles J 1989 application/zip https://dx.doi.org/10.1594/pangaea.744863 https://doi.pangaea.de/10.1594/PANGAEA.744863 en eng PANGAEA https://dx.doi.org/10.2973/odp.proc.sr.105.155.1989 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Composite Core Drilling/drill rig Piston corer Trigger corer Leg105 Joides Resolution Ocean Drilling Program ODP article Collection Supplementary Publication Series of Datasets 1989 ftdatacite https://doi.org/10.1594/pangaea.74486310.2973/odp.proc.sr.105.155.1989 2024-08-01T10:53:32Z Concentrations and activity ratios of uranium and thorium isotopes (234U/238U, 230Th/232Th) were determined at about 5-m intervals through the composite top 22-m sequence of Ocean Drilling Program (ODP) Hole 645 in Baffin Bay and, in the Labrador Sea, at 1-m intervals through the top 11 m of Core 84-030-003 (TWC and P) collected by the Hudson during a preliminary survey of Site 647, and also at about 2-m intervals through the composite top 22-m sequence of Hole 646. In the Labrador Sea, surficial sediments show unsupported 230Th having a 230Th/234U activity ratio of about 3. At Site 647, a regular decrease in the 230Th/232Th activity ratio was observed downcore from about 1.2 (at 1 mbsf) to about 0.4 (at ~8 mbsf), through a sequence spanning over 18O stages 2 through 8. The correlative thorium/uranium chronology and 18O stratigraphy indicate relatively constant sedimentation rates throughout the sequence. At Site 646, down Greenland slope, and at Site 645, in Baffin Bay, highly variable uranium and thorium ... : Supplement to: Causse, Christiane; Vörösmarty, Charles J (1989): Thorium and uranium isotopes in Upper Pleistocene sediments of ODP Sites 645 (Baffin Bay), 646, and 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, 551-560 ... Article in Journal/Newspaper Baffin Bay Baffin Bay Baffin Greenland Labrador Sea DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Composite Core
Drilling/drill rig
Piston corer
Trigger corer
Leg105
Joides Resolution
Ocean Drilling Program ODP
spellingShingle Composite Core
Drilling/drill rig
Piston corer
Trigger corer
Leg105
Joides Resolution
Ocean Drilling Program ODP
Causse, Christiane
Vörösmarty, Charles J
Thorium and uranium isotopes in upper Pleistocene sediments of the Baffin Bay ...
topic_facet Composite Core
Drilling/drill rig
Piston corer
Trigger corer
Leg105
Joides Resolution
Ocean Drilling Program ODP
description Concentrations and activity ratios of uranium and thorium isotopes (234U/238U, 230Th/232Th) were determined at about 5-m intervals through the composite top 22-m sequence of Ocean Drilling Program (ODP) Hole 645 in Baffin Bay and, in the Labrador Sea, at 1-m intervals through the top 11 m of Core 84-030-003 (TWC and P) collected by the Hudson during a preliminary survey of Site 647, and also at about 2-m intervals through the composite top 22-m sequence of Hole 646. In the Labrador Sea, surficial sediments show unsupported 230Th having a 230Th/234U activity ratio of about 3. At Site 647, a regular decrease in the 230Th/232Th activity ratio was observed downcore from about 1.2 (at 1 mbsf) to about 0.4 (at ~8 mbsf), through a sequence spanning over 18O stages 2 through 8. The correlative thorium/uranium chronology and 18O stratigraphy indicate relatively constant sedimentation rates throughout the sequence. At Site 646, down Greenland slope, and at Site 645, in Baffin Bay, highly variable uranium and thorium ... : Supplement to: Causse, Christiane; Vörösmarty, Charles J (1989): Thorium and uranium isotopes in Upper Pleistocene sediments of ODP Sites 645 (Baffin Bay), 646, and 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, 551-560 ...
format Article in Journal/Newspaper
author Causse, Christiane
Vörösmarty, Charles J
author_facet Causse, Christiane
Vörösmarty, Charles J
author_sort Causse, Christiane
title Thorium and uranium isotopes in upper Pleistocene sediments of the Baffin Bay ...
title_short Thorium and uranium isotopes in upper Pleistocene sediments of the Baffin Bay ...
title_full Thorium and uranium isotopes in upper Pleistocene sediments of the Baffin Bay ...
title_fullStr Thorium and uranium isotopes in upper Pleistocene sediments of the Baffin Bay ...
title_full_unstemmed Thorium and uranium isotopes in upper Pleistocene sediments of the Baffin Bay ...
title_sort thorium and uranium isotopes in upper pleistocene sediments of the baffin bay ...
publisher PANGAEA
publishDate 1989
url https://dx.doi.org/10.1594/pangaea.744863
https://doi.pangaea.de/10.1594/PANGAEA.744863
genre Baffin Bay
Baffin Bay
Baffin
Greenland
Labrador Sea
genre_facet Baffin Bay
Baffin Bay
Baffin
Greenland
Labrador Sea
op_relation https://dx.doi.org/10.2973/odp.proc.sr.105.155.1989
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.74486310.2973/odp.proc.sr.105.155.1989
_version_ 1810433082975584256