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Lecture 14 Tomography
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Body waves In the interior Of the Earth’s body P is direct P wave in mantle PcP is a reflection from the core Angle of incidence = Angle of reflection
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P arrives at about 7.7 minutes after the origin of the earthquake
PcP arrives at 9.7 minutes
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P shadow and S shadow were the original evidence for a
liquid outer core. P wave gets refracted downwards because of low P velocity in core. S has zero velocity in outer core.
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Positron emission tomography (PET scan)
MRI (magnetic resonance imaging) CAT Scan [computerized axial tomography (CAT) scan. A CT scanner directs a series of X-ray pulses through the body. ] CT was discovered independently by a British engineer named Sir Godfrey Hounsfield and Dr. Alan Cormack. It has become a mainstay for diagnosing medical diseases. For their work, Hounsfield and Cormack were jointly awarded the Nobel Prize in 1979. Positron emission tomography (PET) is a nuclear medicine medical imaging technique which produces a three-dimensional image or map of functional processes in the body. The system detects pairs of gamma rays emitted indirectly by a positron-emitting radioisotope, which is introduced into the body on a metabolically active molecule.
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MRI 20 Tesla (Earth’s field 50000 nT
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Travel time= distanc/velocity
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Theoretical Tomography
The Radon transform is an integral transform whose inverse is used to reconstruct images from medical CT scans.
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Seismic tomography uses earthquakes (or shots) to image lateral
heterogeneity in the Earth’s interior.
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Tomography beneath Yellowstone Caldera
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Tomography shows shallow asthenosphere
beneath Kenya dome on east African Rift
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Tomography of the mantle and inner core.
(from John Woodhouse) (from Adam Dziewonski) Tomography of the mantle and inner core. Note Africa and Pacific Super Plumes
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Tomography
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Major curculation in the mantle
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UCSD Global Tomographic models
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Slab graveyard ma
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Laboratory Experiments
Lava Lamp Shows plumes rising
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Two deep plumes Two shallow plumes
Montelli et al., Science 2004
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Deep plumes
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Shallow plumes
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Plumes from Montelli et al., 2004
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From Albarede and VanderHilst
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Tomography of Furnace Creek Fault zone
Steps: 1. Pick 48x48 arrivals using RAS24.exe Save as ascii 2. Use linear velocity background model V=a+bz analytic solutions for T, X 3. Find average a b that fit data 4. Find nearest node points on 5 m grid for rays 5. Back project residuals along rays to form tomogram
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Fit of background model
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Rays One shot Analytic for V=a+bz= z m/s
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Shot at 12 th geophone 55 m.
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Rays from all 48 shots
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Rays interpolated onto 48x48 5 meter grid
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Hit count at each grid node
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Tomogram
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Tomogram after stacking travel times Note loader.m shows velocities
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Axis (no vertical exaggeration) image view of tomogram
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