Radially anisotropic structure beneath the Shikoku Basin from broadband surface wave analysis of ocean bottom seismometer records-Reference-Cited by-同舟云学术

Radially anisotropic structure beneath the Shikoku Basin from broadband surface wave analysis of ocean bottom seismometer records

Author:

Takeo A.¹,Nishida K.¹,Isse T.¹,Kawakatsu H.¹,Shiobara H.¹,Sugioka H.²,Kanazawa T.³

Affiliation:

1. Earthquake Research Institute; University of Tokyo; Tokyo Japan

2. Institute For Research on Earth Evolution; Japan Agency for Marine-Earth Science and Technology; Yokosuka Japan

3. National Research Institute for Earth Science and Disaster Prevention; Tsukuba Japan

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Link

Reference79 articles.

1. Space and time spectra of stationary stochastic waves, with special reference to microtremors;Aki;Bull. Earthquake Res. Inst.,1957

2. Phase velocity of low waves in Japan (Part 1): Love waves from the Aleutian Shock of March 9, 1957;Aki;Bull. Earthquake Res. Inst.,1963

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