Gutenberg, B. (1934) The structure of the Earth's crust as indicated by seismological data. In: Proceedings of the Fifth Pacific Science Congress. Vol.2. University of Toronto Press , Toronto, Canada, pp. 2511-2521. https://resolver.caltech.edu/CaltechAUTHORS:20200127-103126506
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Abstract
When an earthquake occurs, two different kinds of waves are generated: waves which travel through the interior of the earth (space waves), and waves whose energy is propagated chiefly along surfaces (surface waves). The records of both kinds of waves can be used to study certain physical properties of the several layers of the earth, especially of the earth's crust.
| Item Type: | Book Section | ||||
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| Additional Information: | © 1934 Pacific Science Association. | ||||
| Other Numbering System: |
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| Record Number: | CaltechAUTHORS:20200127-103126506 | ||||
| Persistent URL: | https://resolver.caltech.edu/CaltechAUTHORS:20200127-103126506 | ||||
| Usage Policy: | No commercial reproduction, distribution, display or performance rights in this work are provided. | ||||
| ID Code: | 100939 | ||||
| Collection: | CaltechAUTHORS | ||||
| Deposited By: | Tony Diaz | ||||
| Deposited On: | 28 Jan 2020 19:34 | ||||
| Last Modified: | 23 Nov 2022 22:24 |
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