1 / 28

The Earth s Structure from Travel Times

Seismology and the Earth's Deep Interior. Spherically Symmetric Structure . Parameters which can be determined for a reference model- P-wave velocity - S-wave velocity- Density- Attenuation (Q) - Anisotropic parameters - Bulk modulus Ks - rigidity m- pressure

cricket
Download Presentation

The Earth s Structure from Travel Times

An Image/Link below is provided (as is) to download presentation Download Policy: Content on the Website is provided to you AS IS for your information and personal use and may not be sold / licensed / shared on other websites without getting consent from its author. Content is provided to you AS IS for your information and personal use only. Download presentation by click this link. While downloading, if for some reason you are not able to download a presentation, the publisher may have deleted the file from their server. During download, if you can't get a presentation, the file might be deleted by the publisher.

E N D

Presentation Transcript


    1. Seismology and the Earth’s Deep Interior The Earth’s Structure from Travel Times

    2. Seismology and the Earth’s Deep Interior Spherically Symmetric Structure

    3. Seismology and the Earth’s Deep Interior PREM: velocities and density

    4. Seismology and the Earth’s Deep Interior PREM: Attenuation

    5. Seismology and the Earth’s Deep Interior Earth’s Regions and Fractional Mass

    6. Seismology and the Earth’s Deep Interior The Earth’s Crust: Travel Times

    7. Seismology and the Earth’s Deep Interior The Earth’s Crust: Minerals and Velocities

    8. Seismology and the Earth’s Deep Interior The Earth’s Crust: Crustal Types

    9. Seismology and the Earth’s Deep Interior The Earth’s Crust: Refraction Studies

    10. Seismology and the Earth’s Deep Interior The Earth’s crust: Crustal Types

    11. Seismology and the Earth’s Deep Interior The Earth’s crust: Crustal Types

    12. Seismology and the Earth’s Deep Interior The Earth’s crust: Crustal Types

    13. Seismology and the Earth’s Deep Interior The Earth’s Upper Mantle: Athenosphere

    14. Seismology and the Earth’s Deep Interior Upper Mantle: Phase transitions

    15. Seismology and the Earth’s Deep Interior Upper Mantle: Discontinuities

    16. Seismology and the Earth’s Deep Interior Upper Mantle: Phase transitions

    17. Seismology and the Earth’s Deep Interior Upper Mantle: Anisotropy

    18. Seismology and the Earth’s Deep Interior Lower Mantle: D”

    19. Seismology and the Earth’s Deep Interior Lower Mantle: Diffracted Waves

    20. Seismology and the Earth’s Deep Interior The Earth’s Core

    21. Seismology and the Earth’s Deep Interior The Earth’s Core: Multiples

    22. Seismology and the Earth’s Deep Interior Upper mantle: 3-D structure

    23. Seismology and the Earth’s Deep Interior Mid-mantle: 3-D structure

    24. Seismology and the Earth’s Deep Interior Lower Mantle: 3-D structure

    25. Seismology and the Earth’s Deep Interior Global Cut: 3-D structure

    26. Seismology and the Earth’s Deep Interior Geodynamic Modelling: Subduction Zones

    27. Seismology and the Earth’s Deep Interior Geodynamic Modelling: Subduction Zones

    28. Seismology and the Earth’s Deep Interior Geodynamic Modelling: Plumes

    29. Seismology and the Earth’s Deep Interior The Earth’s Structure: Summary

More Related