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.

Bibliographic Details
Published in:Journal of Glaciology
Main Author: Holdsworth, G.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1975
Subjects:
Earth-Surface Processes
Journal of Glaciology
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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spelling 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
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