On crustal structure deduced from seismic time‐distance curves
Abstract The numerical computation of the time‐distance curves for several quite different velocity‐depth functions shows that first arrivals are not sufficient to determine the velocity‐depth function. Minor second‐order fluctuations in velocity superimposed on a general velocity gradient in the cr...
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| Published in: | New Zealand Journal of Geology and Geophysics |
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| Format: | Article |
| Language: | English |
| Published: |
Taylor & Francis
1962
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| Online Access: | https://doi.org/10.1080/00288306.1962.10423096 |
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