Spectral structure in the Earth's microseismic background between 20 and 40 seconds

Bulletin of the Seismological Society of America

Volumn 88, Issue 3, 1998, Pages 744-757

  Holcomb, L Gary ^a  

^a U S GEOLOGICAL SURVEY   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

EARTH MOTION; MICROSEISMIC BACKGROUND; SEASONALITY;

EID: 0031753265     PISSN: 00371106     EISSN: None     Source Type: Journal    
DOI: None     Document Type: Article

References (7)

1. Båth, M. (1974). Spectral Analysis in Geophysics, Elsevier, Amsterdam.
2. Bernard, P. and L. Martel (1990). A possible origin of 26 s microseisms, Phys. Earth Planet. Interiors 63, 229-231.
3. Haubrich, R. A., W. H. Munk, and F. E. Snodgrass (1963). Comparative spectra of microseisms and swell, Bull. Seism. Soc. Am. 53, 27-37.
4. Holcomb, L. G. (1980). Microseisms: a twenty-six-second spectral line in long-period Earth motion, Bull. Seism. Soc. Am. 70, 1055-1070.
5. Oliver, J. (1962). A worldwide storm of microseisms with period of about 27 seconds, Bull. Seism. Soc. Am. 52, 507-517.
6. Oliver, J. (1963). Additional evidence relating to "a worldwide storm of microseisms with period of about 27 seconds," Bull. Seism. Soc. Am. 53, 681-685.
7. Press, W. H., B. P. Flannery, S. A. Teukolski, and W. T. Vetterling (1986). Numerical Recipes, Cambridge U Press, New York.