Crustal Structure from Teleseismic Converted Phases Observed

at a Short-Period Array in Panamint Range, California.

Ying Zhou & Robert A Phinney

Geosciences, Princeton University , Princeton, NJ 08540

---

Next: SSCDP Reflection/refraction profiles

Geological setting of Panamint Range

SSCDP reflection/refraction Profile

SSCDP Converted Phases

Data Processing

Data Collection

Data Processing - I

Data Processing II - Off Azimuth

Off-Azimuth Arrivals

Data Processing -III Beam-forming

Receiver Function Analysis

Receiver Function Method

Simple Case : Ps Phase

Receiver Function Migration

Migrated Receiver Functions

Receiver Functions in Contours

Forward Modeling - I

Forward Modleing - II

Shear Wave Splitting

Shear Wave Splitting Observation

Shear wave Splitting Parameters

Moho Ps Phase splitting Parameters

Mid-Crust Negative PS Splitting Parameters

Conclusion

Conclusion

Appendix : De-convolution

Appendix : Deconvolution -I

Appendix : Deconvolution -II

Stacked Resolution Functions