Measurement of Small Strain-Rates over Short Time Periods
A laser interferometer has been used to measure small relative displacements between two reference points spaced up to 99.76 m apart and fixed in an ice surface. Strain-rates of order 10 −11 s −1 can be detected easily within a 24 h period and possibly within an 8 h period.
Published in: | Journal of Glaciology |
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Format: | Article in Journal/Newspaper |
Language: | English |
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Cambridge University Press (CUP)
1975
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Online Access: | http://dx.doi.org/10.1017/s0022143000021791 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000021791 |
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crcambridgeupr:10.1017/s0022143000021791 2024-03-03T08:46:02+00:00 Measurement of Small Strain-Rates over Short Time Periods Holdsworth, G. 1975 http://dx.doi.org/10.1017/s0022143000021791 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000021791 en eng Cambridge University Press (CUP) Journal of Glaciology volume 14, issue 71, page 317-324 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1975 crcambridgeupr https://doi.org/10.1017/s0022143000021791 2024-02-08T08:47:47Z A laser interferometer has been used to measure small relative displacements between two reference points spaced up to 99.76 m apart and fixed in an ice surface. Strain-rates of order 10 −11 s −1 can be detected easily within a 24 h period and possibly within an 8 h period. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Journal of Glaciology 14 71 317 324 |
institution |
Open Polar |
collection |
Cambridge University Press |
op_collection_id |
crcambridgeupr |
language |
English |
topic |
Earth-Surface Processes |
spellingShingle |
Earth-Surface Processes Holdsworth, G. Measurement of Small Strain-Rates over Short Time Periods |
topic_facet |
Earth-Surface Processes |
description |
A laser interferometer has been used to measure small relative displacements between two reference points spaced up to 99.76 m apart and fixed in an ice surface. Strain-rates of order 10 −11 s −1 can be detected easily within a 24 h period and possibly within an 8 h period. |
format |
Article in Journal/Newspaper |
author |
Holdsworth, G. |
author_facet |
Holdsworth, G. |
author_sort |
Holdsworth, G. |
title |
Measurement of Small Strain-Rates over Short Time Periods |
title_short |
Measurement of Small Strain-Rates over Short Time Periods |
title_full |
Measurement of Small Strain-Rates over Short Time Periods |
title_fullStr |
Measurement of Small Strain-Rates over Short Time Periods |
title_full_unstemmed |
Measurement of Small Strain-Rates over Short Time Periods |
title_sort |
measurement of small strain-rates over short time periods |
publisher |
Cambridge University Press (CUP) |
publishDate |
1975 |
url |
http://dx.doi.org/10.1017/s0022143000021791 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000021791 |
genre |
Journal of Glaciology |
genre_facet |
Journal of Glaciology |
op_source |
Journal of Glaciology volume 14, issue 71, page 317-324 ISSN 0022-1430 1727-5652 |
op_doi |
https://doi.org/10.1017/s0022143000021791 |
container_title |
Journal of Glaciology |
container_volume |
14 |
container_issue |
71 |
container_start_page |
317 |
op_container_end_page |
324 |
_version_ |
1792501849319800832 |