Shear-wave Velocity Profiling Using Microtremors on Jeju Island, Korea
To reveal shear-wave velocity ( vs ) structures of Jeju Island in Korea,the spatial autocorrelation method was applied to microtremors recorded at five sites using four broadband seismometers.Shear-wave velocities were derived by inverting the dispersion curves of fundamental mode.The inversion models around the periphery of Mt.Halla indicate the existence of a low-velocity layer (LVL) beneath the extrusive volcanic outcrops of Quaternary age.This LVL correlates with Pleistocene marine sediments of the Seoguipo and U Formations that were sampled in nearby wells.Beneath the LVL,vs increases gradually with depth in welded tuffs that overlie a Cretaceous-Paleogene granite.
Ki Young Kim
Department of Geophysics, Kangwon National University, Chuncheon, Korea
国际会议
长沙
英文
205-209
2012-06-15(万方平台首次上网日期,不代表论文的发表时间)