Synthetic Lg Attenuation on Moho Structure and Group Velocity on Source Depth
Abstract
The regional phase Lg has been the subject of many studies due to its ability to reliably estimate source magnitude and to characterize crustal attenuation, however, the relationship between effective Lg Q and the true intrinsic attenuation of the crust is not well understood. We are working to investigate this relationship by conducting a number of numerical experiments to better understand the nature of Lg scattering attenuation for different type of crustal models. We have partitioned our models by 8-nodes hexahedral meshes with SPECFEM3D-Cartesian which is based on the Spectral Element Method. We have used a time step of 0.01 s to make the simulation stable at high frequencies sufficient enough for our study (about 1.0 Hz). It takes about 50 hours for each model running with 324 processors to generate the waveforms. Then we calculate the effective Lg Q with a Two-Station Method. In order to test our method, we have calculated effective Lg Q tomography for a 2-D model with laterally varying intrinsic attenuation and layered velocity. The tomography result matches the input attenuation model very well. We studied effective Lg Q of models with different Moho structures (flat and with a step) and found that Moho step would lead to lower effective Lg Q than that of flat Moho. Furthermore, we have studied the effective Lg Q tomography of model with 3-D Moho structure and found that effective Lg Q is lower at the area of Moho depth changing than that of flat Moho. This is likely caused by scattering attenuation. We have also modeled the group velocity delay of high frequency (1.0 Hz) Lg, which appears to be dependent on source depth (6km, 10km, 15km and 30km). We have found that the Lg energy arrives later for shallow sources than that of deeper sources which is consistent with prior studies. In the future, we plan to conduct more 3-D attenuation models to investigate azimuthally dependent effective Lg Q.
- Publication:
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AGU Fall Meeting Abstracts
- Pub Date:
- December 2016
- Bibcode:
- 2016AGUFM.S31C2786H
- Keywords:
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- 5104 Fracture and flow;
- PHYSICAL PROPERTIES OF ROCKSDE: 7212 Earthquake ground motions and engineering seismology;
- SEISMOLOGYDE: 7215 Earthquake source observations;
- SEISMOLOGYDE: 7290 Computational seismology;
- SEISMOLOGY