Bulk mineral assemblage of sediment core PS72/413-3 determined via full pattern QXRD
The XRD data has been gained from pulverized and homogenized samples each centimeter of core PS72/413-3 GKG by AWI personal at AWI core labs supervised by Drs. Jutta Wollenburg and Jens Matthiessen. XRD raw measurements were run at Crystallography, Geosciences, University of Bremen in 2016-2017. Mea...
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Format: | Dataset |
Language: | English |
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PANGAEA
2022
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Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.945048 https://doi.org/10.1594/PANGAEA.945048 |
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ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.945048 |
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record_format |
openpolar |
institution |
Open Polar |
collection |
PANGAEA - Data Publisher for Earth & Environmental Science |
op_collection_id |
ftpangaea |
language |
English |
topic |
Amerasian Basin Ankerite Ankerite-Dolomite Apatite Aragonite Arctic Ocean ARK-XXIII/3 Barite Calcite Comment DEPTH sediment/rock Dolomite d-value Full Pattern Quantification with QUAX software Giant box corer GKG Gypsum Iron oxides Phyllosilicate Polarstern PS72 PS72/413-3 Pyrite FeS2 Quartz Quartz/Phyllosillicates ratio Sample code/label Siderite X-ray diffraction (Philips X'Pert Pro) XRD |
spellingShingle |
Amerasian Basin Ankerite Ankerite-Dolomite Apatite Aragonite Arctic Ocean ARK-XXIII/3 Barite Calcite Comment DEPTH sediment/rock Dolomite d-value Full Pattern Quantification with QUAX software Giant box corer GKG Gypsum Iron oxides Phyllosilicate Polarstern PS72 PS72/413-3 Pyrite FeS2 Quartz Quartz/Phyllosillicates ratio Sample code/label Siderite X-ray diffraction (Philips X'Pert Pro) XRD Vogt, Christoph Bulk mineral assemblage of sediment core PS72/413-3 determined via full pattern QXRD |
topic_facet |
Amerasian Basin Ankerite Ankerite-Dolomite Apatite Aragonite Arctic Ocean ARK-XXIII/3 Barite Calcite Comment DEPTH sediment/rock Dolomite d-value Full Pattern Quantification with QUAX software Giant box corer GKG Gypsum Iron oxides Phyllosilicate Polarstern PS72 PS72/413-3 Pyrite FeS2 Quartz Quartz/Phyllosillicates ratio Sample code/label Siderite X-ray diffraction (Philips X'Pert Pro) XRD |
description |
The XRD data has been gained from pulverized and homogenized samples each centimeter of core PS72/413-3 GKG by AWI personal at AWI core labs supervised by Drs. Jutta Wollenburg and Jens Matthiessen. XRD raw measurements were run at Crystallography, Geosciences, University of Bremen in 2016-2017. Measurement conditions: Philips X'Pert Diffractometer, Cu radiation, fixed divergence, secoundary Ni filter, 3-85 ° 2theta, 0.0016° step size, 100 sec calculated step time. XRD mineral assemblage determination were subsequently gained through the QUAX full pattern quantitative determination software (see Vogt et al. 2002 at Pangaea methods wiki). The software allows for differentiation of all carbonate minerals incl. Mg-rich calcite. For comparison reasons the d-value for Mg-rich calcite is also given. A QXRD investigation allows for not only identification of mineral content but also for detailing authigenic vs. allochthonous minerals, transport of detrital input to the sediment core and the interpretation of the transport processes and the local environment as well as the paleoceanographic reconstruction of the region. Sediment ages are given through the below mentioned data sets. |
format |
Dataset |
author |
Vogt, Christoph |
author_facet |
Vogt, Christoph |
author_sort |
Vogt, Christoph |
title |
Bulk mineral assemblage of sediment core PS72/413-3 determined via full pattern QXRD |
title_short |
Bulk mineral assemblage of sediment core PS72/413-3 determined via full pattern QXRD |
title_full |
Bulk mineral assemblage of sediment core PS72/413-3 determined via full pattern QXRD |
title_fullStr |
Bulk mineral assemblage of sediment core PS72/413-3 determined via full pattern QXRD |
title_full_unstemmed |
Bulk mineral assemblage of sediment core PS72/413-3 determined via full pattern QXRD |
title_sort |
bulk mineral assemblage of sediment core ps72/413-3 determined via full pattern qxrd |
publisher |
PANGAEA |
publishDate |
2022 |
url |
https://doi.pangaea.de/10.1594/PANGAEA.945048 https://doi.org/10.1594/PANGAEA.945048 |
op_coverage |
LATITUDE: 80.277900 * LONGITUDE: -178.515100 * DATE/TIME START: 2008-09-24T13:29:00 * DATE/TIME END: 2008-09-24T13:29:00 * MINIMUM DEPTH, sediment/rock: 0.00 m * MAXIMUM DEPTH, sediment/rock: 0.38 m |
long_lat |
ENVELOPE(-178.515100,-178.515100,80.277900,80.277900) |
genre |
Arctic Arctic Ocean Berichte zur Polarforschung Polar Research Polarforschung Reports on polar research |
genre_facet |
Arctic Arctic Ocean Berichte zur Polarforschung Polar Research Polarforschung Reports on polar research |
op_relation |
Andrews, John T; Vogt, Christoph (2020): Variations in felsic- versus mafic-sources in the Western Nordic Seas during MIS 1 to MIS 4. Marine Geology, 424, 106164, https://doi.org/10.1016/j.margeo.2020.106164 Vogt, Christoph (1997): Zeitliche und räumliche Verteilung von Mineralvergesellschaftungen in spätquartären Sedimenten des Arktische Ozeans und ihre Nützlichkeit als Klimaindikatoren während der Glazial/Interglazial-Wechsel (Regional and temporal variations of mineral assemblages in Arctic Ocean sediments as climate indicator during glacial/interglacial changes). Berichte zur Polarforschung = Reports on Polar Research, 251, 309 pp, https://doi.org/10.2312/BzP_0251_1997 Vogt, Christoph; Knies, Jochen; Spielhagen, Robert F; Stein, Ruediger (2001): Detailed mineralogical evidence for two nearly identical glacial/deglacial cycles and Atlantic Water advection to the Arctic Ocean during the last 90,000 years. Global and Planetary Change, QUEEN special issue, 31(1-4), 23-44, https://doi.org/10.1016/S0921-8181(01)00111-4 Vogt, Christoph; Lauterjung, Jörg; Fischer, Reinhard (2002): Investigation of the Clay Fraction (<2 μm) of the Clay Minerals Society Reference Clays. Clays and Clay Minerals, 50(3), 388-400, https://doi.org/10.1346/000986002760833765 Wollenburg, Jutta Erika; Matthiessen, Jens; Vogt, Christoph; Nehrke, Gernot; Grotheer, Hendrik; Wilhelms-Dick, Dorothee; Mollenhauer, Gesine (2023): Omnipresent authigenic carbonates distort Arctic radiocarbon chronology [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.938246 https://doi.pangaea.de/10.1594/PANGAEA.945048 https://doi.org/10.1594/PANGAEA.945048 |
op_rights |
CC-BY-4.0: Creative Commons Attribution 4.0 International Access constraints: unrestricted info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.1594/PANGAEA.94504810.1016/j.margeo.2020.10616410.2312/BzP_0251_199710.1016/S0921-8181(01)00111-410.1346/00098600276083376510.1594/PANGAEA.938246 |
_version_ |
1810293059496181760 |
spelling |
ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.945048 2024-09-15T17:51:13+00:00 Bulk mineral assemblage of sediment core PS72/413-3 determined via full pattern QXRD Vogt, Christoph LATITUDE: 80.277900 * LONGITUDE: -178.515100 * DATE/TIME START: 2008-09-24T13:29:00 * DATE/TIME END: 2008-09-24T13:29:00 * MINIMUM DEPTH, sediment/rock: 0.00 m * MAXIMUM DEPTH, sediment/rock: 0.38 m 2022 text/tab-separated-values, 699 data points https://doi.pangaea.de/10.1594/PANGAEA.945048 https://doi.org/10.1594/PANGAEA.945048 en eng PANGAEA Andrews, John T; Vogt, Christoph (2020): Variations in felsic- versus mafic-sources in the Western Nordic Seas during MIS 1 to MIS 4. Marine Geology, 424, 106164, https://doi.org/10.1016/j.margeo.2020.106164 Vogt, Christoph (1997): Zeitliche und räumliche Verteilung von Mineralvergesellschaftungen in spätquartären Sedimenten des Arktische Ozeans und ihre Nützlichkeit als Klimaindikatoren während der Glazial/Interglazial-Wechsel (Regional and temporal variations of mineral assemblages in Arctic Ocean sediments as climate indicator during glacial/interglacial changes). Berichte zur Polarforschung = Reports on Polar Research, 251, 309 pp, https://doi.org/10.2312/BzP_0251_1997 Vogt, Christoph; Knies, Jochen; Spielhagen, Robert F; Stein, Ruediger (2001): Detailed mineralogical evidence for two nearly identical glacial/deglacial cycles and Atlantic Water advection to the Arctic Ocean during the last 90,000 years. Global and Planetary Change, QUEEN special issue, 31(1-4), 23-44, https://doi.org/10.1016/S0921-8181(01)00111-4 Vogt, Christoph; Lauterjung, Jörg; Fischer, Reinhard (2002): Investigation of the Clay Fraction (<2 μm) of the Clay Minerals Society Reference Clays. Clays and Clay Minerals, 50(3), 388-400, https://doi.org/10.1346/000986002760833765 Wollenburg, Jutta Erika; Matthiessen, Jens; Vogt, Christoph; Nehrke, Gernot; Grotheer, Hendrik; Wilhelms-Dick, Dorothee; Mollenhauer, Gesine (2023): Omnipresent authigenic carbonates distort Arctic radiocarbon chronology [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.938246 https://doi.pangaea.de/10.1594/PANGAEA.945048 https://doi.org/10.1594/PANGAEA.945048 CC-BY-4.0: Creative Commons Attribution 4.0 International Access constraints: unrestricted info:eu-repo/semantics/openAccess Amerasian Basin Ankerite Ankerite-Dolomite Apatite Aragonite Arctic Ocean ARK-XXIII/3 Barite Calcite Comment DEPTH sediment/rock Dolomite d-value Full Pattern Quantification with QUAX software Giant box corer GKG Gypsum Iron oxides Phyllosilicate Polarstern PS72 PS72/413-3 Pyrite FeS2 Quartz Quartz/Phyllosillicates ratio Sample code/label Siderite X-ray diffraction (Philips X'Pert Pro) XRD dataset 2022 ftpangaea https://doi.org/10.1594/PANGAEA.94504810.1016/j.margeo.2020.10616410.2312/BzP_0251_199710.1016/S0921-8181(01)00111-410.1346/00098600276083376510.1594/PANGAEA.938246 2024-07-24T02:31:34Z The XRD data has been gained from pulverized and homogenized samples each centimeter of core PS72/413-3 GKG by AWI personal at AWI core labs supervised by Drs. Jutta Wollenburg and Jens Matthiessen. XRD raw measurements were run at Crystallography, Geosciences, University of Bremen in 2016-2017. Measurement conditions: Philips X'Pert Diffractometer, Cu radiation, fixed divergence, secoundary Ni filter, 3-85 ° 2theta, 0.0016° step size, 100 sec calculated step time. XRD mineral assemblage determination were subsequently gained through the QUAX full pattern quantitative determination software (see Vogt et al. 2002 at Pangaea methods wiki). The software allows for differentiation of all carbonate minerals incl. Mg-rich calcite. For comparison reasons the d-value for Mg-rich calcite is also given. A QXRD investigation allows for not only identification of mineral content but also for detailing authigenic vs. allochthonous minerals, transport of detrital input to the sediment core and the interpretation of the transport processes and the local environment as well as the paleoceanographic reconstruction of the region. Sediment ages are given through the below mentioned data sets. Dataset Arctic Arctic Ocean Berichte zur Polarforschung Polar Research Polarforschung Reports on polar research PANGAEA - Data Publisher for Earth & Environmental Science ENVELOPE(-178.515100,-178.515100,80.277900,80.277900) |