Herdmechanische Vorgänge bei einigen zirkumpazifischen Erdbeben
Earthquake mechan'sms can be determined by a method given by P. Byerly and later developed by J. H. Hodgson and his collaborators. By a comparison with the tectonics of the earthquake region, it is possible in most cases to decide which of the two nodal planes represents the fault plane. As a c...
| Published in: | Tellus A: Dynamic Meteorology and Oceanography |
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| Main Author: | |
| Format: | Article in Journal/Newspaper |
| Language: | unknown |
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Stockholm University Press
1957
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| Subjects: | |
| Online Access: | http://dx.doi.org/10.3402/tellusa.v9i1.9061 https://account.a.tellusjournals.se/index.php/su-j-tadmo/article/download/3636/6769 |