DOI: 10.1785/bssa0490040379. The second shear mode of continental Rayleigh waves

The second shear mode of continental Rayleigh waves

10.1785/bssa0490040379

Crossref journal-article

Seismological Society of America (SSA)

Bulletin of the Seismological Society of America (790)

Abstract

Abstract Waves of the Rayleigh type corresponding to the fundamental and first shear modes for the continental crust-mantle system have been identified on seismograms previously. In this paper, waves corresponding to the second shear mode are identified for two paths, one from the Belgian Congo to Pietermaritzburg, South Africa; the other from Oklahoma to Palisades, New York. Comparison of the dispersion of these waves with theoretical dispersion for several crust-mantle models demonstrates the increase in resolving power of this method of obtaining crustal structure when data for several modes are available. There are small but measurable differences in the velocity structures averaged along these two paths.

Bibliography

Oliver, J., Dorman, J., & Sutton, G. (1959). The second shear mode of continental Rayleigh waves. Bulletin of the Seismological Society of America, 49(4), 379â389.

Authors 3

Jack Oliver (first)
James Dorman (additional)
George Sutton (additional)

References 10 Referenced 23

10.1785/BSSA0480010033 / Bull. Seism. Soc. Am. / Normal Modes of Continental Surface Waves by Oliver (1958)
{'issue': 'No. 4', 'key': '2021052617341177100_BIB2', 'article-title': 'The Oklahoma Earthquake of April 9, 1952', 'volume': 'Vol. 46', 'author': 'Miller', 'year': '1956', 'journal-title': 'Bull. Seism. Soc. Am.'} / Bull. Seism. Soc. Am. / The Oklahoma Earthquake of April 9, 1952 by Miller (1956)
{'key': '2021052617341177100_BIB3', 'author': 'Dorman'} by Dorman
10.1785/BSSA0470030187 / Bull. Seism. Soc. Am. / Higher Modes of Continental Rayleigh Waves by Oliver (1957)
10.1785/BSSA0420030219 / Bull. Seism. Soc. Am. / Two Slow Surface Waves across North America by Press (1952)
10.1785/BSSA0480040339 / Bull. Seism. Soc. Am. / The Effect of Surficial Sedimentary Layers on Continental Surface Waves by Oliver (1958)
10.1785/BSSA0460020097 / Bull. Seism. Soc. Am. / Crustal Structure and Surface-Wave Dispersion in Africa by Press (1956)
{'key': '2021052617341177100_BIB7A'}
{'key': '2021052617341177100_BIB7B'}
10.1785/BSSA0460040293 / Bull. Seism. Soc. Am. / Crustal Structure in the Transvaal by Gane (1956)

Dates

Type	When
Created	4 years, 3 months ago (May 26, 2021, 2:54 p.m.)
Deposited	4 years, 3 months ago (May 26, 2021, 2:54 p.m.)
Indexed	3 years ago (Aug. 9, 2022, 8:49 p.m.)
Issued	65 years, 10 months ago (Oct. 1, 1959)
Published	65 years, 10 months ago (Oct. 1, 1959)
Published Online	65 years, 10 months ago (Oct. 1, 1959)
Published Print	65 years, 10 months ago (Oct. 1, 1959)

Funders 0

None

BibTeX

@article{Oliver_1959, title={The second shear mode of continental Rayleigh waves}, volume={49}, ISSN={0037-1106}, url={http://dx.doi.org/10.1785/bssa0490040379}, DOI={10.1785/bssa0490040379}, number={4}, journal={Bulletin of the Seismological Society of America}, publisher={Seismological Society of America (SSA)}, author={Oliver, Jack and Dorman, James and Sutton, George}, year={1959}, month=oct, pages={379–389} }

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