Expedition Menu
1. Introduction
2. The Question
3. Funding
4. Study Area
5. Background
6. Seismogenic Zone
7. Chief Scientists
8. The Journey
9. Ship Tour
10. Leaving Port
11. Seismic Method
12. Seismic Source
13. Seismic Recording
14. 3-D Acquisition
15. Life at Sea
16. In the Lab
17. Time to Depart
18. Data Processing
19. The 3-D Volume
20. Interpretation
21. Your Turn
22. Comparison
23, Publication
24. IODP Drilling
This material is based
upon work supported
by the
National Science Foundation
under
Grant No. 0633234
NanTroSEIZE in 3-D
Imaging an Active Plate Boundary Fault
20. Seismic Interpretation
Learning to Interpret Seismic Data
- Trench sediments and Shikoku Basin sediments carried into trench on the subducting oceanic crust (yellow).
- Frontal thrust zone, which is the most eastward (oceanward) series of thrusts. These are presumably the youngest thrusts, but not the only active thrust faults in the prism.
- Offscraped sediments of the accretionary prism (blue)
- Kumano forearc basin sediments (light green)
- Top of the subducting oceanic crust (pink).
- Subducting sediments of Shikoku Basin sediments (yellow).
- Decollement (active) including Seismogenic Zone along the plate interface (boundary)
- Mega-splay fault, separating the young portion of accretionary prism from older accretionary prism, located under the sediment of the Kumano forearc basin.
