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(see also Seismic Methods: Refraction.

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Presentation on theme: "(see also Seismic Methods: Refraction."— Presentation transcript:

1 (see also http://www.mines.edu/fs_home/tboyd/GP311/MODULES/SEIS/main.html)n Seismic Methods: Refraction

2 Seismic Waves Body Surface P S Love Rayleigh

3 Seismic Wave Speeds MaterialP wave Velocity (m/s)S wave Velocity (m/s) Air332 Water1400-1500 Petroleum1300-1400 Steel61003500 Concrete36002000 Granite5500-59002800-3000 Basalt64003200 Sandstone1400-4300700-2800 Limestone5900-61002800-3000 Sand (Unsaturated)200-100080-400 Sand (Saturated)800-2200320-880 Clay1000-2500400-1000 Glacial Till (Saturated)1500-2500600-1000

4 Reflection and Refraction sin  1 = sin  3 = Vp 1 Vs 1 sin  2 = sin  4 = Vs 2 Vp 2 p (ray parameter)

5 Critical Refraction

6 Seismic Refraction Waves passing from slow to fast medium

7 Reflection & Refraction 0 200 400 T, msec Direct Reflected Refracted

8 Refraction Analysis (flat): Velocity estimation

9 Depth from TT curve

10 Structure from TT curve

11 Refraction: One layer case

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14 Refraction: 3 layer case

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19 Engineering Quad 1/27/00 12 gauge source 1m geophone spacing, 1 m minimum offset

20 Data from Treman (11/2/05)

21 Engineering Quad 1/27/00 12 gauge source 1m geophone spacing, 1 m minimum offset SHOT *

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23 Seismic Raytracing (forward modeling) http://www.scielo.cl/scielo.php?pid=S0716-02082003000100006&script=sci_arttext&tlng=en

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