A scanning electron microscope technique for identifying the mineralogy of dust in ice cores
Dust particles in an ice core from East Rongbuk Glacier on the northern slope of Qomolangma (Mount Everest; 288010 N, 868580 E; 6518 m a.s.l.), central Himalaya, have been identified as mica using a combination of scanning electron microscope-based techniques and energy-dispersive X-ray spectroscopy...
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ftdartmouthcoll:oai:digitalcommons.dartmouth.edu:facoa-1105 2023-07-16T03:59:00+02:00 A scanning electron microscope technique for identifying the mineralogy of dust in ice cores Obbard, Rachel Baker, Ian Prior, David 2011-01-01T08:00:00Z https://digitalcommons.dartmouth.edu/facoa/106 http://www.igsoc.org:8080/journal/57/203/j10j131.pdf unknown Dartmouth Digital Commons https://digitalcommons.dartmouth.edu/facoa/106 http://www.igsoc.org:8080/journal/57/203/j10j131.pdf Dartmouth Scholarship Earth Sciences Engineering text 2011 ftdartmouthcoll 2023-06-28T10:37:31Z Dust particles in an ice core from East Rongbuk Glacier on the northern slope of Qomolangma (Mount Everest; 288010 N, 868580 E; 6518 m a.s.l.), central Himalaya, have been identified as mica using a combination of scanning electron microscope-based techniques and energy-dispersive X-ray spectroscopy to identify the elements present, and electron backscatter diffraction to identify the crystal type. This technique for identifying individual crystalline dust particles in samples of glacial ice could be especially useful in the future for identifying water-soluble crystals in ice, for studying the strain history (glaciotectonics) of basal ice or in studies of ice–mica composites used as analogs of quartz-mica rocks. Text ice core Dartmouth Digital Commons (Dartmouth College) |
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Dartmouth Digital Commons (Dartmouth College) |
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Earth Sciences Engineering |
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Earth Sciences Engineering Obbard, Rachel Baker, Ian Prior, David A scanning electron microscope technique for identifying the mineralogy of dust in ice cores |
topic_facet |
Earth Sciences Engineering |
description |
Dust particles in an ice core from East Rongbuk Glacier on the northern slope of Qomolangma (Mount Everest; 288010 N, 868580 E; 6518 m a.s.l.), central Himalaya, have been identified as mica using a combination of scanning electron microscope-based techniques and energy-dispersive X-ray spectroscopy to identify the elements present, and electron backscatter diffraction to identify the crystal type. This technique for identifying individual crystalline dust particles in samples of glacial ice could be especially useful in the future for identifying water-soluble crystals in ice, for studying the strain history (glaciotectonics) of basal ice or in studies of ice–mica composites used as analogs of quartz-mica rocks. |
format |
Text |
author |
Obbard, Rachel Baker, Ian Prior, David |
author_facet |
Obbard, Rachel Baker, Ian Prior, David |
author_sort |
Obbard, Rachel |
title |
A scanning electron microscope technique for identifying the mineralogy of dust in ice cores |
title_short |
A scanning electron microscope technique for identifying the mineralogy of dust in ice cores |
title_full |
A scanning electron microscope technique for identifying the mineralogy of dust in ice cores |
title_fullStr |
A scanning electron microscope technique for identifying the mineralogy of dust in ice cores |
title_full_unstemmed |
A scanning electron microscope technique for identifying the mineralogy of dust in ice cores |
title_sort |
scanning electron microscope technique for identifying the mineralogy of dust in ice cores |
publisher |
Dartmouth Digital Commons |
publishDate |
2011 |
url |
https://digitalcommons.dartmouth.edu/facoa/106 http://www.igsoc.org:8080/journal/57/203/j10j131.pdf |
genre |
ice core |
genre_facet |
ice core |
op_source |
Dartmouth Scholarship |
op_relation |
https://digitalcommons.dartmouth.edu/facoa/106 http://www.igsoc.org:8080/journal/57/203/j10j131.pdf |
_version_ |
1771546421694038016 |