DECIPHERING THE FINEST IMPRINT OF GLACIAL EROSION: OBJECTIVE ANALYSIS OF STRIAE PATTERNS ON BEDROCK

The aim of this study is to compare the efficiency of different mathematical and statistical geometrical methods applied to characterise the orientation distribution of striae on bedrock for deciphering the finest imprint of glacial erosion. The involved methods include automatic image analysis tech...

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Main Authors: Piet Stroeven, Arjen Peter Stroeven, Jing Hu, Jean-Louis Chermant, Michel Coster
Format: Article
Language:English
Published: Slovenian Society for Stereology and Quantitative Image Analysis 2011-05-01
Series:Image Analysis and Stereology
Subjects:
Online Access:http://www.ias-iss.org/ojs/IAS/article/view/781
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spelling doaj-c53afe51a3b844faa066e9fcc9a1b6372020-11-24T23:24:07ZengSlovenian Society for Stereology and Quantitative Image AnalysisImage Analysis and Stereology1580-31391854-51652011-05-0124313514310.5566/ias.v24.p135-143753DECIPHERING THE FINEST IMPRINT OF GLACIAL EROSION: OBJECTIVE ANALYSIS OF STRIAE PATTERNS ON BEDROCKPiet StroevenArjen Peter StroevenJing HuJean-Louis ChermantMichel CosterThe aim of this study is to compare the efficiency of different mathematical and statistical geometrical methods applied to characterise the orientation distribution of striae on bedrock for deciphering the finest imprint of glacial erosion. The involved methods include automatic image analysis techniques of Fast Fourier Transform (FFT), and the experimental investigations by means of Saltikov's directed secants analysis (rose of intersection densities), applied to digital and analogue images of the striae pattern, respectively. In addition, the experimental data were compared with the modelling results made on the basis of Underwood's concept of linear systems in a plane. The experimental and modelling approaches in the framework of stereology yield consistent results. These results reveal that stereological methods allow a reliable and efficient delineation of different families of glacial striae from a complex record imprinted in bedrock.http://www.ias-iss.org/ojs/IAS/article/view/781Fast Fourier Transformorientation distributionrose of intersection densitiesstriae patternsUnderwood concept
collection DOAJ
language English
format Article
sources DOAJ
author Piet Stroeven
Arjen Peter Stroeven
Jing Hu
Jean-Louis Chermant
Michel Coster
spellingShingle Piet Stroeven
Arjen Peter Stroeven
Jing Hu
Jean-Louis Chermant
Michel Coster
DECIPHERING THE FINEST IMPRINT OF GLACIAL EROSION: OBJECTIVE ANALYSIS OF STRIAE PATTERNS ON BEDROCK
Image Analysis and Stereology
Fast Fourier Transform
orientation distribution
rose of intersection densities
striae patterns
Underwood concept
author_facet Piet Stroeven
Arjen Peter Stroeven
Jing Hu
Jean-Louis Chermant
Michel Coster
author_sort Piet Stroeven
title DECIPHERING THE FINEST IMPRINT OF GLACIAL EROSION: OBJECTIVE ANALYSIS OF STRIAE PATTERNS ON BEDROCK
title_short DECIPHERING THE FINEST IMPRINT OF GLACIAL EROSION: OBJECTIVE ANALYSIS OF STRIAE PATTERNS ON BEDROCK
title_full DECIPHERING THE FINEST IMPRINT OF GLACIAL EROSION: OBJECTIVE ANALYSIS OF STRIAE PATTERNS ON BEDROCK
title_fullStr DECIPHERING THE FINEST IMPRINT OF GLACIAL EROSION: OBJECTIVE ANALYSIS OF STRIAE PATTERNS ON BEDROCK
title_full_unstemmed DECIPHERING THE FINEST IMPRINT OF GLACIAL EROSION: OBJECTIVE ANALYSIS OF STRIAE PATTERNS ON BEDROCK
title_sort deciphering the finest imprint of glacial erosion: objective analysis of striae patterns on bedrock
publisher Slovenian Society for Stereology and Quantitative Image Analysis
series Image Analysis and Stereology
issn 1580-3139
1854-5165
publishDate 2011-05-01
description The aim of this study is to compare the efficiency of different mathematical and statistical geometrical methods applied to characterise the orientation distribution of striae on bedrock for deciphering the finest imprint of glacial erosion. The involved methods include automatic image analysis techniques of Fast Fourier Transform (FFT), and the experimental investigations by means of Saltikov's directed secants analysis (rose of intersection densities), applied to digital and analogue images of the striae pattern, respectively. In addition, the experimental data were compared with the modelling results made on the basis of Underwood's concept of linear systems in a plane. The experimental and modelling approaches in the framework of stereology yield consistent results. These results reveal that stereological methods allow a reliable and efficient delineation of different families of glacial striae from a complex record imprinted in bedrock.
topic Fast Fourier Transform
orientation distribution
rose of intersection densities
striae patterns
Underwood concept
url http://www.ias-iss.org/ojs/IAS/article/view/781
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