| Reference Type | Journal (article/letter/editorial) |
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| Title | P-Wave Residuals in Western Canada |
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| Journal | Canadian Journal of Earth Sciences |
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| Authors | Roebroek, E. J. | Author |
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| Nyland, E. | Author |
| Year | 1975 (February 1) | Volume | 12 |
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| Issue | 2 |
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| Publisher | Canadian Science Publishing |
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| DOI | doi:10.1139/e75-017Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 474347 | Long-form Identifier | mindat:1:5:474347:1 |
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| GUID | 0 |
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| Full Reference | Roebroek, E. J., Nyland, E. (1975) P-Wave Residuals in Western Canada. Canadian Journal of Earth Sciences, 12 (2) 174-181 doi:10.1139/e75-017 |
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| Plain Text | Roebroek, E. J., Nyland, E. (1975) P-Wave Residuals in Western Canada. Canadian Journal of Earth Sciences, 12 (2) 174-181 doi:10.1139/e75-017 |
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| In | (1975, February) Canadian Journal of Earth Sciences Vol. 12 (2) Canadian Science Publishing |
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| Abstract/Notes | A study of over 1500 P-wave phases which pass, for the most part, through the upper mantle beneath Western Canada, shows that there is no significant lateral variation in P-wave velocity structure beneath Western Canada, and that the Wiggins and Helmberger model for the Western regions of the United States does not fit the data for Western Canada.One possible interpretation of the data for Western Canada is closer to the classical Herrin model of P-wave velocity as a function of depth than it is to the Wiggins and Helmberger A model. |
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