U-Th isotope systematics and light stable isotope data of carbonate enriched sediments at MASOX and HyBIS sites (methane seepage off Svalbard) from JAGO dives during cruise Maria S. Merian MSM21/4 ...
Values with # mark highly unreliable ages characterized by uncertainties larger than the deduced age or even dominated by 230Th correction values as well as isochron approaches based just on 2-point reference lines. Therefore, the latter may not provide any proof for the petrographic postulation of...
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ftdatacite:10.1594/pangaea.825734 2024-09-15T18:38:27+00:00 U-Th isotope systematics and light stable isotope data of carbonate enriched sediments at MASOX and HyBIS sites (methane seepage off Svalbard) from JAGO dives during cruise Maria S. Merian MSM21/4 ... Liebetrau, Volker Krause, Stefan 2014 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.825734 https://doi.pangaea.de/10.1594/PANGAEA.825734 en eng PANGAEA https://dx.doi.org/10.1594/pangaea.824947 https://dx.doi.org/10.1126/science.1246298 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Event label Latitude of event Longitude of event DEPTH, sediment/rock Depth, top/min Depth, bottom/max Sample code/label Location Description Sample mass non-silicates, total Age, dated Age, error Uranium-238 Error, absolute Thorium-232 Uranium-234/Uranium-238 activity ratio Uranium-234/Uranium-238 activity ratio, error, absolute Thorium-230/Thorium-232 activity ratio Uranium-238/Thorium-232 activity ratio Thorium-230/Uranium-234 activity ratio δ13C, carbonate δ18O, carbonate Carbonates Age model Submersible JAGO MC-ICP-MS, isotope dilution Calculated Mass spectrometer, Finnigan, MAT 253 X-ray diffractometry Philips PW1710 MSM21/4 Maria S. Merian Dataset dataset 2014 ftdatacite https://doi.org/10.1594/pangaea.82573410.1594/pangaea.82494710.1126/science.1246298 2024-07-03T13:10:33Z Values with # mark highly unreliable ages characterized by uncertainties larger than the deduced age or even dominated by 230Th correction values as well as isochron approaches based just on 2-point reference lines. Therefore, the latter may not provide any proof for the petrographic postulation of cogenetic origin.Uncertainties presented on 2 sigma level.HyBIS U-measurements were performed on Quadrupole Inductively Coupled Plasma Mass Spectrometer (Q-ICP-MS) on limited precision level.Note 1: The sample weight represents the analysed amount dissolved in 4 N Acetic Acid and 2.25 N HNO3 (marked by -2), respectively, at room temperature over 2 hours. Remaining material was 2 x centrifuged, dried down and weighed for recalculation of the dissolved sample weight.Note 2: The equivalent percentage of the analysed non-silicate fraction represented by the sample weight. X-ray diffraction analyses indicated aragonite as the main non-silicate and easily dissolvable phase. ... Dataset Svalbard DataCite |
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collection |
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op_collection_id |
ftdatacite |
language |
English |
topic |
Event label Latitude of event Longitude of event DEPTH, sediment/rock Depth, top/min Depth, bottom/max Sample code/label Location Description Sample mass non-silicates, total Age, dated Age, error Uranium-238 Error, absolute Thorium-232 Uranium-234/Uranium-238 activity ratio Uranium-234/Uranium-238 activity ratio, error, absolute Thorium-230/Thorium-232 activity ratio Uranium-238/Thorium-232 activity ratio Thorium-230/Uranium-234 activity ratio δ13C, carbonate δ18O, carbonate Carbonates Age model Submersible JAGO MC-ICP-MS, isotope dilution Calculated Mass spectrometer, Finnigan, MAT 253 X-ray diffractometry Philips PW1710 MSM21/4 Maria S. Merian |
spellingShingle |
Event label Latitude of event Longitude of event DEPTH, sediment/rock Depth, top/min Depth, bottom/max Sample code/label Location Description Sample mass non-silicates, total Age, dated Age, error Uranium-238 Error, absolute Thorium-232 Uranium-234/Uranium-238 activity ratio Uranium-234/Uranium-238 activity ratio, error, absolute Thorium-230/Thorium-232 activity ratio Uranium-238/Thorium-232 activity ratio Thorium-230/Uranium-234 activity ratio δ13C, carbonate δ18O, carbonate Carbonates Age model Submersible JAGO MC-ICP-MS, isotope dilution Calculated Mass spectrometer, Finnigan, MAT 253 X-ray diffractometry Philips PW1710 MSM21/4 Maria S. Merian Liebetrau, Volker Krause, Stefan U-Th isotope systematics and light stable isotope data of carbonate enriched sediments at MASOX and HyBIS sites (methane seepage off Svalbard) from JAGO dives during cruise Maria S. Merian MSM21/4 ... |
topic_facet |
Event label Latitude of event Longitude of event DEPTH, sediment/rock Depth, top/min Depth, bottom/max Sample code/label Location Description Sample mass non-silicates, total Age, dated Age, error Uranium-238 Error, absolute Thorium-232 Uranium-234/Uranium-238 activity ratio Uranium-234/Uranium-238 activity ratio, error, absolute Thorium-230/Thorium-232 activity ratio Uranium-238/Thorium-232 activity ratio Thorium-230/Uranium-234 activity ratio δ13C, carbonate δ18O, carbonate Carbonates Age model Submersible JAGO MC-ICP-MS, isotope dilution Calculated Mass spectrometer, Finnigan, MAT 253 X-ray diffractometry Philips PW1710 MSM21/4 Maria S. Merian |
description |
Values with # mark highly unreliable ages characterized by uncertainties larger than the deduced age or even dominated by 230Th correction values as well as isochron approaches based just on 2-point reference lines. Therefore, the latter may not provide any proof for the petrographic postulation of cogenetic origin.Uncertainties presented on 2 sigma level.HyBIS U-measurements were performed on Quadrupole Inductively Coupled Plasma Mass Spectrometer (Q-ICP-MS) on limited precision level.Note 1: The sample weight represents the analysed amount dissolved in 4 N Acetic Acid and 2.25 N HNO3 (marked by -2), respectively, at room temperature over 2 hours. Remaining material was 2 x centrifuged, dried down and weighed for recalculation of the dissolved sample weight.Note 2: The equivalent percentage of the analysed non-silicate fraction represented by the sample weight. X-ray diffraction analyses indicated aragonite as the main non-silicate and easily dissolvable phase. ... |
format |
Dataset |
author |
Liebetrau, Volker Krause, Stefan |
author_facet |
Liebetrau, Volker Krause, Stefan |
author_sort |
Liebetrau, Volker |
title |
U-Th isotope systematics and light stable isotope data of carbonate enriched sediments at MASOX and HyBIS sites (methane seepage off Svalbard) from JAGO dives during cruise Maria S. Merian MSM21/4 ... |
title_short |
U-Th isotope systematics and light stable isotope data of carbonate enriched sediments at MASOX and HyBIS sites (methane seepage off Svalbard) from JAGO dives during cruise Maria S. Merian MSM21/4 ... |
title_full |
U-Th isotope systematics and light stable isotope data of carbonate enriched sediments at MASOX and HyBIS sites (methane seepage off Svalbard) from JAGO dives during cruise Maria S. Merian MSM21/4 ... |
title_fullStr |
U-Th isotope systematics and light stable isotope data of carbonate enriched sediments at MASOX and HyBIS sites (methane seepage off Svalbard) from JAGO dives during cruise Maria S. Merian MSM21/4 ... |
title_full_unstemmed |
U-Th isotope systematics and light stable isotope data of carbonate enriched sediments at MASOX and HyBIS sites (methane seepage off Svalbard) from JAGO dives during cruise Maria S. Merian MSM21/4 ... |
title_sort |
u-th isotope systematics and light stable isotope data of carbonate enriched sediments at masox and hybis sites (methane seepage off svalbard) from jago dives during cruise maria s. merian msm21/4 ... |
publisher |
PANGAEA |
publishDate |
2014 |
url |
https://dx.doi.org/10.1594/pangaea.825734 https://doi.pangaea.de/10.1594/PANGAEA.825734 |
genre |
Svalbard |
genre_facet |
Svalbard |
op_relation |
https://dx.doi.org/10.1594/pangaea.824947 https://dx.doi.org/10.1126/science.1246298 |
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.82573410.1594/pangaea.82494710.1126/science.1246298 |
_version_ |
1810482853255839744 |