Entrainment, transport and concentration of meteorites in polar ice sheets
Glaciers and ice sheets act as slow-moving conveyancing systems for material added to both their upper and lower surfaces. Because the transit time for most materials is extremely long the ice acts as a major global storage facility. The effects of horizontal and vertical motions on the flow pattern...
Main Author: | |
---|---|
Format: | Other/Unknown Material |
Language: | unknown |
Published: |
1986
|
Subjects: | |
Online Access: | http://hdl.handle.net/2060/19860019345 |
id |
ftnasantrs:oai:casi.ntrs.nasa.gov:19860019345 |
---|---|
record_format |
openpolar |
spelling |
ftnasantrs:oai:casi.ntrs.nasa.gov:19860019345 2023-05-15T13:53:27+02:00 Entrainment, transport and concentration of meteorites in polar ice sheets Drewry, D. J. Unclassified, Unlimited, Publicly available JAN 1, 1986 application/pdf http://hdl.handle.net/2060/19860019345 unknown Document ID: 19860019345 Accession ID: 86N28817 http://hdl.handle.net/2060/19860019345 No Copyright CASI ASTROPHYSICS Lunar and Planetary Inst. International Workshop on Antarctic Meteorites; p 37-47 1986 ftnasantrs 2016-06-11T22:52:12Z Glaciers and ice sheets act as slow-moving conveyancing systems for material added to both their upper and lower surfaces. Because the transit time for most materials is extremely long the ice acts as a major global storage facility. The effects of horizontal and vertical motions on the flow patterns of Antarctic ice sheets are summarized. The determination of the source areas of meteorites and their transport paths is a problem of central importance since it relates not only directly to concentration mechanisms but also to the wider issues in glaciology and meteorites. The ice and snow into which a meteorite falls, and which moves with it to the concentration area, encodes information about the infall area. The principle environmental conditions being former elevation, temperature (also related to elevation), and age of the ice. This encoded information could be used to identify the infall area. Other/Unknown Material Antarc* Antarctic NASA Technical Reports Server (NTRS) Antarctic |
institution |
Open Polar |
collection |
NASA Technical Reports Server (NTRS) |
op_collection_id |
ftnasantrs |
language |
unknown |
topic |
ASTROPHYSICS |
spellingShingle |
ASTROPHYSICS Drewry, D. J. Entrainment, transport and concentration of meteorites in polar ice sheets |
topic_facet |
ASTROPHYSICS |
description |
Glaciers and ice sheets act as slow-moving conveyancing systems for material added to both their upper and lower surfaces. Because the transit time for most materials is extremely long the ice acts as a major global storage facility. The effects of horizontal and vertical motions on the flow patterns of Antarctic ice sheets are summarized. The determination of the source areas of meteorites and their transport paths is a problem of central importance since it relates not only directly to concentration mechanisms but also to the wider issues in glaciology and meteorites. The ice and snow into which a meteorite falls, and which moves with it to the concentration area, encodes information about the infall area. The principle environmental conditions being former elevation, temperature (also related to elevation), and age of the ice. This encoded information could be used to identify the infall area. |
format |
Other/Unknown Material |
author |
Drewry, D. J. |
author_facet |
Drewry, D. J. |
author_sort |
Drewry, D. J. |
title |
Entrainment, transport and concentration of meteorites in polar ice sheets |
title_short |
Entrainment, transport and concentration of meteorites in polar ice sheets |
title_full |
Entrainment, transport and concentration of meteorites in polar ice sheets |
title_fullStr |
Entrainment, transport and concentration of meteorites in polar ice sheets |
title_full_unstemmed |
Entrainment, transport and concentration of meteorites in polar ice sheets |
title_sort |
entrainment, transport and concentration of meteorites in polar ice sheets |
publishDate |
1986 |
url |
http://hdl.handle.net/2060/19860019345 |
op_coverage |
Unclassified, Unlimited, Publicly available |
geographic |
Antarctic |
geographic_facet |
Antarctic |
genre |
Antarc* Antarctic |
genre_facet |
Antarc* Antarctic |
op_source |
CASI |
op_relation |
Document ID: 19860019345 Accession ID: 86N28817 http://hdl.handle.net/2060/19860019345 |
op_rights |
No Copyright |
_version_ |
1766258551545659392 |