Published January 1948
| Published
Journal Article
Open
A possible layer for the transmission of fast P waves from surface disturbances
- Creators
- Wood, Harry O.
Abstract
Unless the principle of isostasy is rejected, in all its somewhat variant forms, there is some minimum depth beneath the surface of the land and sea, a relatively small depth, where the pressure due to the superincumbent rock, water, and atmosphere is the same everywhere.
Additional Information
© 1948 by the Seismological Society of America. Manuscript received for publication, July 14, 1947. The writer wishes to make acknowledgments to J. A. Anderson, L. H. Adams, B. Gutenberg, and C. F. Richter, who have read the manuscript and made critical suggestions, and to G. D. Louderback and P. Byerly also, but none of them should bear any responsibility for any shortcomings which remain.Attached Files
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Additional details
- Eprint ID
- 113441
- Resolver ID
- CaltechAUTHORS:20220214-612221000
- Created
-
2022-02-15Created from EPrint's datestamp field
- Updated
-
2022-02-15Created from EPrint's last_modified field
- Other Numbering System Name
- Caltech Division of Geological Sciences
- Other Numbering System Identifier
- 452-B