Crustal Seismic Anisotropy in Shandong
Abstract
Based on the seismic data of near-field source from Shandong Seismic Network, the study obtained the shear-wave splitting parameters from multiple stations. The results show that dominant directions of polarizations of fast shear-waves reflect the spatial distribution characteristics of tectonic stress in this area, CHD and LIS stations show 2 dominant direction, it reveals that the crustal seismic anisotropy in Shandong area is constrained by regional stress background, local failure and structure.
Keywords
Shear-Wave Splitting, Polarization, Seismic Anisotropy, Tectonic Stress, Shandong Area
DOI
10.12783/dtmse/icmsea/mce2017/10866
10.12783/dtmse/icmsea/mce2017/10866
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