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; 28deg 01' N, 58deg 00' E; 6518m a.s.l.), central Himalaya, have been identified as mica using a combination of scanning electron microscope-based techniques and energy-dispersive X-r...
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ftdartmouthcoll:oai:digitalcommons.dartmouth.edu:facoa-1065 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 application/pdf https://digitalcommons.dartmouth.edu/facoa/66 https://digitalcommons.dartmouth.edu/context/facoa/article/1065/viewcontent/68.pdf unknown Dartmouth Digital Commons https://digitalcommons.dartmouth.edu/facoa/66 https://digitalcommons.dartmouth.edu/context/facoa/article/1065/viewcontent/68.pdf Dartmouth Scholarship Glaciology text 2011 ftdartmouthcoll 2023-06-28T10:42:43Z Dust particles in an ice core from East Rongbuk Glacier on the northern slope of Qomolangma (Mount Everest; 28deg 01' N, 58deg 00' E; 6518m 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 icemica 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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Glaciology |
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Glaciology Obbard, Rachel Baker, Ian Prior, David A scanning electron microscope technique for identifying the mineralogy of dust in ice cores |
topic_facet |
Glaciology |
description |
Dust particles in an ice core from East Rongbuk Glacier on the northern slope of Qomolangma (Mount Everest; 28deg 01' N, 58deg 00' E; 6518m 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 icemica 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/66 https://digitalcommons.dartmouth.edu/context/facoa/article/1065/viewcontent/68.pdf |
genre |
ice core |
genre_facet |
ice core |
op_source |
Dartmouth Scholarship |
op_relation |
https://digitalcommons.dartmouth.edu/facoa/66 https://digitalcommons.dartmouth.edu/context/facoa/article/1065/viewcontent/68.pdf |
_version_ |
1771546420697890816 |