10. Seismic Stratigraphy

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Examples of prograding configuration pattern Mitchum et al. (1977), p.127 Sequence <strong>Stratigraphy</strong> Department of Earth Sciences National Central Univ., Taiwan Prepared by Dr. Andrew T. Lin 38
4. Chaotic: This pattern is interpreted to represent a disordered arrangement of reflection surfaces owing to penecontemporan eous, softsediment deformation, or possibly to deposition of strata in a variable, high-energy environment. Mitchum et al. (1977), p.129 Sequence <strong>Stratigraphy</strong> Department of Earth Sciences National Central Univ., Taiwan Prepared by Dr. Andrew T. Lin 39
Page 1 and 2: 10. Seismic Stratigraphy Reflection
Page 3 and 4: Main body of seismic data (courtesy
Page 5 and 6: ◎ Nature of a reflection Velocity
Page 7 and 8: ♥ Polarity Positive RC produces a
Page 9 and 10: 10.2 Resolution of seismic data A.
Page 11 and 12: Thin-bed effect or tuning Reflector
Page 13 and 14: B. Lateral resolution The seismic e
Page 15 and 16: 10.3 Chronostratigraphic significan
Page 17 and 18: 10.4 Seismic sequence analysis The
Page 19 and 20: An idealized sequence Vail (1987) S
Page 21 and 22: Apparent truncation is the terminat
Page 23 and 24: Toplap is the termination of inclin
Page 25 and 26: Examples of onlap (one kind of base
Page 27 and 28: Examples of toplap (Mitchum et al.,
Page 29 and 30: Practical: On the following figure,
Page 31 and 32: 10.5 Seismic facies analysis Seismi
Page 33 and 34: 2. Parallelism of reflection cycles
Page 35 and 36: 2. Divergent: Divergent configurati
Page 37: Examples of prograding configuratio
Page 41 and 42: External forms of seismic facies un
Page 43 and 44: Interpretation of lithofacies and d
Page 45 and 46: Summary of seismic facies character
Page 47 and 48: Summary of seismic facies character

10. Seismic Stratigraphy

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