1. I. Basic Techniques in Structural Geology Field measurements and mapping Terminology on folds and folds Stereographic projections From maps to cross-sections Growth Strata Fault related folds Seismic Imaging

2. Twiss and Moores, ‘Structural geology’, Chapter 2. C.M.R. Fowler, ‘The Solid Earth, An introduction to Global Geophysics’ Shaw, Connors and Suppe, ‘Seismic Interpretation of Contractional Fault- related Folds’ (AAPG Seismic Altlas, #53) http://principles.ou.edu/seismic_explo/refle ct/reflect.html

3. ‘Snell’s laws’ - There is no energy refracted if i>i c, where the critical angle is defined by i c = sin -1 (V 1 /V 2 ) Rock Vp (km/s) Granite 5.0 Basalt 5.5 Limestone 6.0 Sandstone 4.2 Shale 2.5

4. Seismic Imaging Techniques Seismic reflection Seismic refraction geophonesSource Direct Reflected Refracted time icic icic

5. Seismic Imaging Techniques Seismic refraction Seismic reflection geophonesSource V2V2 V1V1 Travel time of P wave Critical distance: x c Crossover distance: X cross V 1 < V 2 icic icic

6. Seismic Imaging Techniques Seismic refraction Seismic reflection geophonesSource V2V2 V1V1 Travel time of P wave Critical distance: x c Crossover distance: X cross V 1 < V 2

7. Seismic Imaging Techniques Seismic refraction Seismic reflection geophonesSource V2V2 V1V1 Travel time of P wave Critical distance: x c Crossover distance: X cross V 1 < V 2

8. Reflection coefficient geophonesSource A typical value for R is 0.001 Seismic Reflection Reflectors reflect contrasts of acoustic impedance: Polarity of reflected wave depends on sign of reflection coefficient

9. Simple ‘zero-offset’ Reflection survey An ‘image’ of the subsurface is obtained by plotting seismograms side by side. Reflections are generally faint The ‘image’ obtained this way is in two-way time, not depth. (to convert to depth the velocity needs to be determined). The cost scales with the number of sources For these reasons it is advantageous to deploy lines of geophones (with a range of ‘offsets’)

10. geophonesSource A B C - t 0 is the two-way normal incidence travel time: - An horizontal reflector generates an hyperbola in time - Velocity, V 1, and depth, z, can be determined by plotting t 2 as function of x 2. Seismic Reflection x z Two-way travel time is: t0t0 Or

11. geophonesSource A B C Seismic Reflection x z Two-way travel time is: t0t0 - t 0 is the two-way normal incidence travel time: - An horizontal reflector generates an hyperbola in time - Velocity, V 1, and depth, z, can be determined by plotting t 2 as function of x 2. Or

13. Common Mid- Point (CMP) Stacking The seismograms corresponding to the various offsets can be corrected to account for the effect of the offset on the arrival time (Normal Move Out), and then stacked to simulate a ‘zero offset’ seismograms with enhanced signal to noise ratio. The Normal Move Out is :

14. In case of multiple layers the t 2 -x 2 plot yields the ‘Root Mean Square velocity’,V RMS, (also called stacking velocity): The equation is used to correct for NMO before stacking. V RMS relates to interval velocity according to Dix’s equation Interval velocities and thicknesses are determined from Common Mid- Point Stacking

15. Unmigrated Seismic Reflection Profile - Seismograms are plotted side by side. - Vertical axis is the two-way travel time - A Common Mid-Point (CMP) stacked profile show records as if shots and geophones were coincident

16. Migration In a stacked profile all reflections are plotted as if they were coming from vertical ray paths. This is a ‘distorted’ view of the sub-surface. Diffractions Migration aims at correcting these distortions and diffractions (assuming that all reflections are in the plane of the vertical section along the geophones line).

17. Distortions

18. Buried focus

19. An example with Synthetic seismograms Distortions

20. Diffractions

22. Still not directly an image of the subsurface. Unmigrated Seismic Reflection ProfileMigrated Seismic Reflection Profile

24. Most Common ‘Artifacts’ Multiples (Sediment/Basement interface or water/sea bottom interface in marine survey) Sideswipes (reflections out of the plane of the section) can mess up the migration process. Incorrectly migrated diffractions (they look like anticlines but are not) Pull-up and Pull-down (not really artifacts)

25. Multiples geophonesSource Primary reflection Time t1t1 2.t 1 First multiple 0

26. Reflection seismic Line DLC9708 (Hopper et al., 1997). Extent of corresponding sparker seismic lines marked by thick line at top. Three first multiples can be seen lower in the section

27. Shortcomings in seismic images of folds Folds can be distorted or only partially imaged in seismic sections. Two common shortcomings are: (1) Overlapping reflections in un- migrated or under-migrated sections; (2) lack of imaging of steeply dipping fold limbs. NB: Note also pullup.

28. (Camerlo&Benson, AAPG, 2006)

31. Deformation since Sueyi Time