Fig. 2: Comparison of the number of grains counted in a sieve analysis
The distribution of ice rafted debris (IRD) is an important parameter in glaciomarine sediments. A simple method is presented allowing the determination of the IRD-content by counting the gravel fraction of the X-radiographs which are generally taken during sarnpling. In comparison with sieve analys...
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Format: | Dataset |
Language: | English |
Published: |
PANGAEA
1987
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Subjects: | |
Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.756793 https://doi.org/10.1594/PANGAEA.756793 |
Summary: | The distribution of ice rafted debris (IRD) is an important parameter in glaciomarine sediments. A simple method is presented allowing the determination of the IRD-content by counting the gravel fraction of the X-radiographs which are generally taken during sarnpling. In comparison with sieve analyses corresponding values are obtained by both methods. However, more information can be made available in a shorter time by this method. |
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