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Lithospheric Structure of the Gulf of California – Salton Trough Region, NARS-Baja Array. Working Group: Robert Clayton, Caltech Don Forsyth, Brown Antonio Gonzalez-Fernandez, CICESE Craig Jones, Colorado Cecillio Rebollar, CICESE Jose Romo-Jones, CICESE. Science Questions :
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Lithospheric Structure of the Gulf of California – Salton Trough Region, NARS-Baja Array Working Group: Robert Clayton, Caltech Don Forsyth, Brown Antonio Gonzalez-Fernandez, CICESE Craig Jones, Colorado Cecillio Rebollar, CICESE Jose Romo-Jones, CICESE
Science Questions: • What is the rifting process and how does it vary from north • to south in the Gulf • What is the role of the remnant slab – where does it exist. • Methods • Map of the Moho from seismic and other geophysical methods. • Map of the lithosphere/asthenosphere boundary. • Velocity Variations from tomography studies. • Flow directions from anisotropy • Current strain from earthquakes • Products • 3D regional-scale velocity model • Earthquake catalogue.
Receiver Functions Lewis et al, 2001 Ichinose et al, 1996
Receiver Functions – Southern California Seismic Network Yan and Clayton, 2006
Crustal Thickness From Surface Waves Yang and Forsyth, 2005
NARS-Baja / RESBAN Array http://www.data.scec.org/NARS-Baja/ April, 2002 – April, 2007
Receiver Functions – Gulf of California Persaud, Perez-Campos and Clayton, 2005
I III Along Peninsula Profiles II Lopez-Pineda et al, 2005
Electrical Profile Romo, Gomez-Trevino, Esparza, Garcia-Abdesiem, and Flores-Luna, 2003
Regional 3D Velocity From Surface Waves and Receiver Functions DiLuccio, Clayton, Persaud, Perez-Campos, 2005
Rayliegh Wave Group Velocity Dispersion Curves for Four Events
3D Regional-scale velocity model for the Gulf of California DiLuccio, Clayton and Persaud, AGU, UGM, 2005
The 2002 Gulf of California Seismic Experiment Lizarralde et al Column
Column Description Top Column Description col 23.456 -117.234 123.0 SAMPLE1 lay 0.0 DEN 2700VS 3.5 DVS 0.015 VP 5.0 DVP 0.015 TOP lay5.0 DEN 2700 DDEN 10.0VS 3.6 VP 6.0 DVP -0.02 lay8.0DEN 2800VS 4.5 VP 7.0 MOHO Moho Interface Names Parameters DEN, DDEN - density VS, DVS - shear velocity VP, DVP - P-wave velocity QS, DQS - S attenuation QP, DQP - P attenuation ???? - anisotropy
Top Moho (lat,lon,z)
Flow Direction From S-Wave Anisotropy – Rayleigh Vs Love Waves 7071-R 7071-L 8081-R 8081-L Initial model Rayleigh waves Love waves
Microseism – 6 sec – station NE81 Noise Correlation Infrasonic – 30-100 sec – NE82
Receiver Functions of Deeper Interfaces Perez-Campos, Persaud and Clayton, UGM, AGU 2004