XRD mineralogy of sediment core JM07-WP-174-GC ...

We employ the quantitative X-ray diffraction method developed by Eberl (2003, 2004). The sediment < 2 mm are spiked by 10% by weight of zincite, milled, and the samples are scanned on a D5000 Siemens X-Ray Diffractometer between 5° and 65° 2-theta with a 0.02° step and a 2-sec count. The resultin...

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Main Authors: Andrews, John T, Stein, Ruediger, Moros, Matthias, Perner, Kerstin
Format: Dataset
Language:English
Published: PANGAEA 2016
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.848749
https://doi.pangaea.de/10.1594/PANGAEA.848749
id ftdatacite:10.1594/pangaea.848749
record_format openpolar
spelling ftdatacite:10.1594/pangaea.848749 2024-09-09T19:48:57+00:00 XRD mineralogy of sediment core JM07-WP-174-GC ... Andrews, John T Stein, Ruediger Moros, Matthias Perner, Kerstin 2016 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.848749 https://doi.pangaea.de/10.1594/PANGAEA.848749 en eng PANGAEA https://pubs.usgs.gov/of/2003/of03-078/ https://pubs.usgs.gov/publication/70026557 https://dx.doi.org/10.1594/pangaea.848769 https://dx.doi.org/10.1111/bor.12169 https://pubs.usgs.gov/of/2003/of03-078/ https://pubs.usgs.gov/publication/70026557 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 DEPTH, sediment/rock Full pattern degree of fit Quartz Microcline Orthoclase Anorthoclase Albite Oligoclase Labradorite Bytownite Anorthite Calcite Dolomite Iron-Dolomite Siderite Halite Ferrotschermakite Diopside Pyrite, FeS2 Magnetite Hematite, Fe2O3 Maghemite Diatoms Chert Non-clay minerals Kaolinite Saponite Smectite Illite Biotite Iron-Chlorite Muscovite Clay minerals Total Gravity corer X-ray diffraction Siemens D5000 JM07-WP Jan Mayen dataset Dataset 2016 ftdatacite https://doi.org/10.1594/pangaea.84874910.1594/pangaea.84876910.1111/bor.12169 2024-08-01T10:30:47Z We employ the quantitative X-ray diffraction method developed by Eberl (2003, 2004). The sediment < 2 mm are spiked by 10% by weight of zincite, milled, and the samples are scanned on a D5000 Siemens X-Ray Diffractometer between 5° and 65° 2-theta with a 0.02° step and a 2-sec count. The resulting 3000 data points are loaded into the Excel macro-program Rockjock v6 (Eberl, 2003) and the weight% of minerals in the sediment mixtures calculated against a suite of 124 "standard" mineral patterns (Eberl, 2003). Finally, the data are normalized to sum to 100% ... Dataset Jan Mayen DataCite Jan Mayen
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic DEPTH, sediment/rock
Full pattern degree of fit
Quartz
Microcline
Orthoclase
Anorthoclase
Albite
Oligoclase
Labradorite
Bytownite
Anorthite
Calcite
Dolomite
Iron-Dolomite
Siderite
Halite
Ferrotschermakite
Diopside
Pyrite, FeS2
Magnetite
Hematite, Fe2O3
Maghemite
Diatoms
Chert
Non-clay minerals
Kaolinite
Saponite
Smectite
Illite
Biotite
Iron-Chlorite
Muscovite
Clay minerals
Total
Gravity corer
X-ray diffraction Siemens D5000
JM07-WP
Jan Mayen
spellingShingle DEPTH, sediment/rock
Full pattern degree of fit
Quartz
Microcline
Orthoclase
Anorthoclase
Albite
Oligoclase
Labradorite
Bytownite
Anorthite
Calcite
Dolomite
Iron-Dolomite
Siderite
Halite
Ferrotschermakite
Diopside
Pyrite, FeS2
Magnetite
Hematite, Fe2O3
Maghemite
Diatoms
Chert
Non-clay minerals
Kaolinite
Saponite
Smectite
Illite
Biotite
Iron-Chlorite
Muscovite
Clay minerals
Total
Gravity corer
X-ray diffraction Siemens D5000
JM07-WP
Jan Mayen
Andrews, John T
Stein, Ruediger
Moros, Matthias
Perner, Kerstin
XRD mineralogy of sediment core JM07-WP-174-GC ...
topic_facet DEPTH, sediment/rock
Full pattern degree of fit
Quartz
Microcline
Orthoclase
Anorthoclase
Albite
Oligoclase
Labradorite
Bytownite
Anorthite
Calcite
Dolomite
Iron-Dolomite
Siderite
Halite
Ferrotschermakite
Diopside
Pyrite, FeS2
Magnetite
Hematite, Fe2O3
Maghemite
Diatoms
Chert
Non-clay minerals
Kaolinite
Saponite
Smectite
Illite
Biotite
Iron-Chlorite
Muscovite
Clay minerals
Total
Gravity corer
X-ray diffraction Siemens D5000
JM07-WP
Jan Mayen
description We employ the quantitative X-ray diffraction method developed by Eberl (2003, 2004). The sediment < 2 mm are spiked by 10% by weight of zincite, milled, and the samples are scanned on a D5000 Siemens X-Ray Diffractometer between 5° and 65° 2-theta with a 0.02° step and a 2-sec count. The resulting 3000 data points are loaded into the Excel macro-program Rockjock v6 (Eberl, 2003) and the weight% of minerals in the sediment mixtures calculated against a suite of 124 "standard" mineral patterns (Eberl, 2003). Finally, the data are normalized to sum to 100% ...
format Dataset
author Andrews, John T
Stein, Ruediger
Moros, Matthias
Perner, Kerstin
author_facet Andrews, John T
Stein, Ruediger
Moros, Matthias
Perner, Kerstin
author_sort Andrews, John T
title XRD mineralogy of sediment core JM07-WP-174-GC ...
title_short XRD mineralogy of sediment core JM07-WP-174-GC ...
title_full XRD mineralogy of sediment core JM07-WP-174-GC ...
title_fullStr XRD mineralogy of sediment core JM07-WP-174-GC ...
title_full_unstemmed XRD mineralogy of sediment core JM07-WP-174-GC ...
title_sort xrd mineralogy of sediment core jm07-wp-174-gc ...
publisher PANGAEA
publishDate 2016
url https://dx.doi.org/10.1594/pangaea.848749
https://doi.pangaea.de/10.1594/PANGAEA.848749
geographic Jan Mayen
geographic_facet Jan Mayen
genre Jan Mayen
genre_facet Jan Mayen
op_relation https://pubs.usgs.gov/of/2003/of03-078/
https://pubs.usgs.gov/publication/70026557
https://dx.doi.org/10.1594/pangaea.848769
https://dx.doi.org/10.1111/bor.12169
https://pubs.usgs.gov/of/2003/of03-078/
https://pubs.usgs.gov/publication/70026557
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.84874910.1594/pangaea.84876910.1111/bor.12169
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