Microtremor measurement was done mainly in the damaged areas in San Francisco and Oakland after the 1989 Loma Prieta earthquake. The observation areas were (1) the Marina District, (2) Cypress Street, (3) the Embarcadero, and (4) South of Market District. Predominant frequency (Fp) and amplification factor (Ap) obtained from a spectral ratio between horizontal and vertical components were evaluated for each observation cite. Difference in the degree of damage in the areas (1) and (4) was coincident with difference in Ap and Fp. Significant difference could not be found in Ap and Fp between the areas (2) and (3)
A study of a limited number of vertical ground motion acceleration-time histories recorded during th...
The recorded response of the Marina District of the City of San Francisco to an aftershock of the 19...
Short-period micro tremor array observation is conducted at five sites in the Tokyo Metropolitan are...
Microtremor measurement was done mainly in the damaged areas in San Francisco and Oakland after the ...
A large earthquake occurred in the Santa Cruz mountains, California, on 17 October 1989, and many st...
The amplification characteristics of earthquake ground motion were investigated based on the Chiba A...
Strong motion records of the Loma Prieta Earthquake of October, 17, 1989 have been analyzed in compa...
Possible use of short-period microtremors is explored for estimating the effects of subsurface soil ...
The nature of strong earthquake ground shaking has been investigated based on a study of 15 accelero...
Strong earthquake ground shaking has been investigated by the study of 15 events recorded in El Cent...
This paper discusses the use of microseism measurement as a tool to predict local site amplification...
The Loma Prieta Earthquake ground motions recorded on Treasure Island, a man-made fill in San Franci...
The 1985 Mexico City earthquake and the 1989 Loma Prieta earthquake provided well-documented evidenc...
The nature of strong earthquake ground shaking has been investigated based on a study of 15 accelero...
The 1985 Michoacan earthquake caused extensive loss of life and severe damages. During the earthquak...
A study of a limited number of vertical ground motion acceleration-time histories recorded during th...
The recorded response of the Marina District of the City of San Francisco to an aftershock of the 19...
Short-period micro tremor array observation is conducted at five sites in the Tokyo Metropolitan are...
Microtremor measurement was done mainly in the damaged areas in San Francisco and Oakland after the ...
A large earthquake occurred in the Santa Cruz mountains, California, on 17 October 1989, and many st...
The amplification characteristics of earthquake ground motion were investigated based on the Chiba A...
Strong motion records of the Loma Prieta Earthquake of October, 17, 1989 have been analyzed in compa...
Possible use of short-period microtremors is explored for estimating the effects of subsurface soil ...
The nature of strong earthquake ground shaking has been investigated based on a study of 15 accelero...
Strong earthquake ground shaking has been investigated by the study of 15 events recorded in El Cent...
This paper discusses the use of microseism measurement as a tool to predict local site amplification...
The Loma Prieta Earthquake ground motions recorded on Treasure Island, a man-made fill in San Franci...
The 1985 Mexico City earthquake and the 1989 Loma Prieta earthquake provided well-documented evidenc...
The nature of strong earthquake ground shaking has been investigated based on a study of 15 accelero...
The 1985 Michoacan earthquake caused extensive loss of life and severe damages. During the earthquak...
A study of a limited number of vertical ground motion acceleration-time histories recorded during th...
The recorded response of the Marina District of the City of San Francisco to an aftershock of the 19...
Short-period micro tremor array observation is conducted at five sites in the Tokyo Metropolitan are...