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Introduction to Geophysics Ali Oncel [email_address] Department of Earth Sciences KFUPM Seismic Reflection 4: Acquisiton, Processing, and Waveform Analysis Introduction to Geophysics-KFUPM
Types of Velocities  Average Velocity  Root mean Square Velocity (RMS)  Interval velocity Previous Lecture Introduction to Geophysics-KFUPM
Example: Disk Formula v 1 =1500 m s -1 v 2 =2000 m s -1 v 3 =2345 m s -1 t 1 =2.14 s t 2 =1.21 s t 3 =1.13 s What is  v rms  at the base of layer 3? Introduction to Geophysics-KFUPM
Introduction to Geophysics-KFUPM
Introduction to Geophysics-KFUPM Fig 5.21 of Lillie
Introduction to Geophysics-KFUPM
“ 12 elephants dancing in unison” (LITHOPROBE, CANADA) A vibrator truck Vibroseis images from the Lithoprobe Project, Canada  www.lithoprobe.ca Introduction to Geophysics-KFUPM
Introduction to Geophysics-KFUPM Fig. 5.23 of Lillie
Reflection and Transmission ,[object Object],[object Object],[object Object],[object Object],[object Object],Introduction to Geophysics-KFUPM From Kearey, Brooks, and Hill, 2002
Reflection and Transmission It becomes for a normally incident ray: ,[object Object],Introduction to Geophysics-KFUPM ,[object Object],T 12   = 2I 1  / (I 1 +I 2 ) T 21   = 2I 2  / (I 2 +I 1 ) Transmission Coefficients
Example: Air-water reflection ρ air   =0; Vp=330 m/s ρ water  =1; Vp=1500m/s R AirWater  = (I Water -I Air ) / (I Air +I Water ) R AirWater  = (I Water -0) / (0+I Water ) R AirWater   = 1 Introduction to Geophysics-KFUPM Air Layer 1 Layer 2
ρ air  =0; Vp=330 m/s ρ water  =1; Vp=1500m/s Example: Water-air reflection R WaterAir   = (I Air -I Water ) / (I Air +I Water ) R WaterAir   = -1 ( A negative reflection coefficient) Introduction to Geophysics-KFUPM Air Water Layer 1 Layer 2
Introduction to Geophysics-KFUPM
Introduction to Geophysics-KFUPM ,[object Object],[object Object],Fig. 5.25 of Lillie
Introduction to Geophysics-KFUPM b) Seismic response for reflection at interface with positive reflection coefficient c) Seismic response for negative reflection coefficient Fig. 5.26 of Lillie a) Input minimum phase and zero phase seismic signals
Introduction to Geophysics-KFUPM High Frequency Input
Introduction to Geophysics-KFUPM Low Frequency Input
Introduction to Geophysics-KFUPM
Introduction to Geophysics-KFUPM
Convolution ,[object Object],[object Object],[object Object],[object Object],Introduction to Geophysics-KFUPM
Source and Earth Response ,[object Object],[object Object],Introduction to Geophysics-KFUPM See pp. 353 of Reynolds, 2002

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ÖNCEL AKADEMİ: INTRODUCTION TO GEOPHYSICS

Notas del editor

  1. qqq
  2. Whether the reflected wave has the same or opposite polarity as the input seismic signal depends on whether the reflection coefficient is positive or negative.
  3. Convolution means replacing each reflection coefficient with the input seismic signal, scaled to the amplitude and polarity of the reflection coefficient.