Gutenberg, B. (1958) Two types of microseisms. Journal of Geophysical Research, 63 (3). pp. 595-597. ISSN 0148-0227. doi:10.1029/JZ063i003p00595. https://resolver.caltech.edu/CaltechAUTHORS:20140807-150207193
|
PDF
- Published Version
See Usage Policy. 113kB |
Use this Persistent URL to link to this item: https://resolver.caltech.edu/CaltechAUTHORS:20140807-150207193
Abstract
In general, microseisms are a nuisance. It is now quite widely agreed that microseisms are channel waves, similar in nature to the Lg and Rg waves. It is not at all unusual to observe microseisms which have traveled over distances of continental proportions. In order to determine the direction from which the microseisms come and to investigate in more detail the characteristics of microseismic disturbances, we established a tri-partite system on Mount Palomar.
| Item Type: | Article | |||||||||
|---|---|---|---|---|---|---|---|---|---|---|
| Related URLs: |
| |||||||||
| Additional Information: | Copyright 1958 by the American Geophysical Union. | |||||||||
| Other Numbering System: |
| |||||||||
| Issue or Number: | 3 | |||||||||
| DOI: | 10.1029/JZ063i003p00595 | |||||||||
| Record Number: | CaltechAUTHORS:20140807-150207193 | |||||||||
| Persistent URL: | https://resolver.caltech.edu/CaltechAUTHORS:20140807-150207193 | |||||||||
| Official Citation: | Gutenberg, B. (1958), Two types of microseisms, J. Geophys. Res., 63(3), 595–597, doi:10.1029/JZ063i003p00595 | |||||||||
| Usage Policy: | No commercial reproduction, distribution, display or performance rights in this work are provided. | |||||||||
| ID Code: | 48201 | |||||||||
| Collection: | CaltechAUTHORS | |||||||||
| Deposited By: | George Porter | |||||||||
| Deposited On: | 07 Aug 2014 22:07 | |||||||||
| Last Modified: | 10 Nov 2021 18:30 |
Repository Staff Only: item control page
