Mineralogy of surface sediment from the Canadian Beaufort Shelf and Amundsen Gulf (Canadian Arctic) ...
For the semi-quantification of the major mineralogical components, bulk sediment XRD scans were processed in the software package X'Pert High-Score Plus (PANalytical) using the Rietveld full-pattern fitting method. This method permits the semi-quantification of whole-sediment mineralogy with a...
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Online Access: | https://dx.doi.org/10.1594/pangaea.866869 https://doi.pangaea.de/10.1594/PANGAEA.866869 |
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ftdatacite:10.1594/pangaea.866869 2024-09-15T17:38:53+00:00 Mineralogy of surface sediment from the Canadian Beaufort Shelf and Amundsen Gulf (Canadian Arctic) ... Gamboa, Adriana Montero-Serrano, Jean-Carlos St-Onge, Guillaume Rochon, André Desiage, Pierre-Arnaud 2016 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.866869 https://doi.pangaea.de/10.1594/PANGAEA.866869 en eng PANGAEA https://dx.doi.org/10.1594/pangaea.866871 https://dx.doi.org/10.1002/2016gc006477 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Event label Station label Latitude of event Longitude of event Elevation of event DEPTH, sediment/rock Zone Difference Goodness of fit Quartz Kalifeldspar Plagioclase Calcite Dolomite Pyroxene Magnetite Iron oxide Phyllosilicate Box corer X-ray diffraction XRD dataset Dataset 2016 ftdatacite https://doi.org/10.1594/pangaea.86686910.1594/pangaea.86687110.1002/2016gc006477 2024-08-01T11:01:20Z For the semi-quantification of the major mineralogical components, bulk sediment XRD scans were processed in the software package X'Pert High-Score Plus (PANalytical) using the Rietveld full-pattern fitting method. This method permits the semi-quantification of whole-sediment mineralogy with a precision of 5-10% for phyllosilicates and 5% for non-phyllosilicates minerals. The quality of the Rietveld fitting procedure was evaluated for the R-profile and goodness-of-fit (GOF). The R-profile quantifies the difference between the observed and calculated patterns, whereas the GOF is the ratio between the R-weighted profile (RWP; best least-squares fit between observed and calculated patterns) and R-expected theoretical (Rexp; best possible value for the residual). ... Dataset Amundsen Gulf DataCite |
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Open Polar |
collection |
DataCite |
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ftdatacite |
language |
English |
topic |
Event label Station label Latitude of event Longitude of event Elevation of event DEPTH, sediment/rock Zone Difference Goodness of fit Quartz Kalifeldspar Plagioclase Calcite Dolomite Pyroxene Magnetite Iron oxide Phyllosilicate Box corer X-ray diffraction XRD |
spellingShingle |
Event label Station label Latitude of event Longitude of event Elevation of event DEPTH, sediment/rock Zone Difference Goodness of fit Quartz Kalifeldspar Plagioclase Calcite Dolomite Pyroxene Magnetite Iron oxide Phyllosilicate Box corer X-ray diffraction XRD Gamboa, Adriana Montero-Serrano, Jean-Carlos St-Onge, Guillaume Rochon, André Desiage, Pierre-Arnaud Mineralogy of surface sediment from the Canadian Beaufort Shelf and Amundsen Gulf (Canadian Arctic) ... |
topic_facet |
Event label Station label Latitude of event Longitude of event Elevation of event DEPTH, sediment/rock Zone Difference Goodness of fit Quartz Kalifeldspar Plagioclase Calcite Dolomite Pyroxene Magnetite Iron oxide Phyllosilicate Box corer X-ray diffraction XRD |
description |
For the semi-quantification of the major mineralogical components, bulk sediment XRD scans were processed in the software package X'Pert High-Score Plus (PANalytical) using the Rietveld full-pattern fitting method. This method permits the semi-quantification of whole-sediment mineralogy with a precision of 5-10% for phyllosilicates and 5% for non-phyllosilicates minerals. The quality of the Rietveld fitting procedure was evaluated for the R-profile and goodness-of-fit (GOF). The R-profile quantifies the difference between the observed and calculated patterns, whereas the GOF is the ratio between the R-weighted profile (RWP; best least-squares fit between observed and calculated patterns) and R-expected theoretical (Rexp; best possible value for the residual). ... |
format |
Dataset |
author |
Gamboa, Adriana Montero-Serrano, Jean-Carlos St-Onge, Guillaume Rochon, André Desiage, Pierre-Arnaud |
author_facet |
Gamboa, Adriana Montero-Serrano, Jean-Carlos St-Onge, Guillaume Rochon, André Desiage, Pierre-Arnaud |
author_sort |
Gamboa, Adriana |
title |
Mineralogy of surface sediment from the Canadian Beaufort Shelf and Amundsen Gulf (Canadian Arctic) ... |
title_short |
Mineralogy of surface sediment from the Canadian Beaufort Shelf and Amundsen Gulf (Canadian Arctic) ... |
title_full |
Mineralogy of surface sediment from the Canadian Beaufort Shelf and Amundsen Gulf (Canadian Arctic) ... |
title_fullStr |
Mineralogy of surface sediment from the Canadian Beaufort Shelf and Amundsen Gulf (Canadian Arctic) ... |
title_full_unstemmed |
Mineralogy of surface sediment from the Canadian Beaufort Shelf and Amundsen Gulf (Canadian Arctic) ... |
title_sort |
mineralogy of surface sediment from the canadian beaufort shelf and amundsen gulf (canadian arctic) ... |
publisher |
PANGAEA |
publishDate |
2016 |
url |
https://dx.doi.org/10.1594/pangaea.866869 https://doi.pangaea.de/10.1594/PANGAEA.866869 |
genre |
Amundsen Gulf |
genre_facet |
Amundsen Gulf |
op_relation |
https://dx.doi.org/10.1594/pangaea.866871 https://dx.doi.org/10.1002/2016gc006477 |
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.86686910.1594/pangaea.86687110.1002/2016gc006477 |
_version_ |
1810475990958211072 |