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Integrated and Comparative Geophysical Studies of Crustal Structure of Pull-apart Basins: The Salton Trough and Death Valley, California Regions
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Crust, Moho
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Crustal Structure (Model)
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Integrated: Integrated: - Receiver Function - Gravity - Magnetic - Pre-existing seismic models
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RF A receiver function is the seismic response of the earth beneath a seismic station to an incoming P-wave. The physical earth property that controls what is observed in a receiver function is the P-to-S impedance structure A receiver function is the seismic response of the earth beneath a seismic station to an incoming P-wave. The physical earth property that controls what is observed in a receiver function is the P-to-S impedance structure http://www.earthscope.org/ http://www.earthscope.org/ http://www.earthscope.org/
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http://www.seis.sc.edu/ears/
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RF
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Gravity http://research.utep.edu/ http://research.utep.edu/ http://research.utep.edu
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Bouguer anomaly map
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Crustal Models Four 2-D crustal models were constructed Four 2-D crustal models were constructed A-A`, B-B`, C-C trend in SW-NE and D-D` trends in NW- SE direction A-A`, B-B`, C-C trend in SW-NE and D-D` trends in NW- SE direction
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http://woodshole.er.usgs.gov/mapit/ http://woodshole.er.usgs.gov/mapit/ http://woodshole.er.usgs.gov/mapit/ http://gmt.soest.hawaii.edu/ http://gmt.soest.hawaii.edu/ http://gmt.soest.hawaii.edu/
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