A theoretical explanation of grain size distributions in explosive rock fragmentation.
We have measured grain size distributions of the results of laboratory decompression explosions of volcanic rock. The resulting distributions can be approximately represented by gamma distributions of weight per cent as a function of [Formula: see text], where d is the grain size in millimetres meas...
| Hlavní autoři: | , |
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| Médium: | Journal article |
| Jazyk: | English |
| Vydáno: |
Royal Society
2016
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