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Introduction to Geophysics Ali Oncel [email_address] Department of Earth Sciences KFUPM Tectonic Interpretation of Seismic Refraction Profiles Introduction to Geophysics-KFUPM
Previous Lecture ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],Introduction to Geophysics-KFUPM
Δ X=10 m ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],0.007 0.01 148 m 45 m 0.01 0.02 0.03 0.04 Introduction to Geophysics-KFUPM 0.01 Second 0.034
[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],Homework due to April 15 Introduction to Geophysics-KFUPM P.C: 1  milisecond is 10^-3 seconds
[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],Problem 3.3 in pp. 127 Berger's book. Using the information in Figure, determine as much as possible about the subsurface geology at the site where the information was recorded. Homework due to April 15 Introduction to Geophysics-KFUPM P.C: 1  milisecond is 10^-3 seconds
Parks and Plates ©2005 Robert J. Lillie Plate Boundaries Introduction to Geophysics-KFUPM
Introduction to Geophysics-KFUPM A. Jon Kimerling Parks and Plates ©2005 Robert J. Lillie Raised Relief Map of North America and Adjacent Oceans
Introduction to Geophysics-KFUPM Due to shallow hot mantle Due to cold lithospheric plate Map of P-wave Velocity (km/s)
Parks and Plates ©2005 Robert J. Lillie Active Continental Rifts Advanced Rifting (Lower Elevations) Early Rifting (Higher Elevations) Introduction to Geophysics-KFUPM National Park Lands
Introduction to Geophysics-KFUPM Map of P-wave Velocity (km/s)
Introduction to Geophysics-KFUPM Crustal thinning due to  Continental rifting Remember that  Red Sea  is a good example for Continental Rifting.  Map of Crustal Thickness (km)
Parks and Plates ©2005 Robert J. Lillie Crustal Thinning at Continental Rifts Introduction to Geophysics-KFUPM As the lithosphere rips apart, the underlying asthenosphere becomes shallow while the crust still fairly thick.  The buoyancy of the shallow asthenosphere and thick crust results in high overall elevation of the Basin.
Crustal Thinning at Continental Rifts Parks and Plates ©2005 Robert J. Lillie Grand Teton National Park, Wyoming Great Basin National Park, Nevada Introduction to Geophysics-KFUPM
Crustal Thinning at Continental Rifts Parks and Plates ©2005 Robert J. Lillie Introduction to Geophysics-KFUPM As the continental crust thins, it is less buoyant.  Elevations  are lower through the region.
Parks and Plates ©2005 Robert J. Lillie Sagauro National Park, Arizona Death Valley National Park, California Crustal Thinning at Continental Rifts Introduction to Geophysics-KFUPM
Parks and Plates ©2005 Robert J. Lillie Crustal Thinning at Continental Rifts Introduction to Geophysics-KFUPM
Parks and Plates ©2005 Robert J. Lillie Salton Sea Gulf of California Crustal Thinning at Continental Rifts Introduction to Geophysics-KFUPM
Continental Rifting  eventually open an  Ocean Basin Parks and Plates ©2005 Robert J. Lillie Introduction to Geophysics-KFUPM Red Sea  is a good example for Continental Rifting  (see pp. 50, Lillie 2005).
Parks and Plates ©2005 Robert J. Lillie Continental Rifting  eventually open an  Ocean Basin Introduction to Geophysics-KFUPM
Parks and Plates ©2005 Robert J. Lillie Continental   Rifting  eventually open an  Ocean Basin Introduction to Geophysics-KFUPM
Parks and Plates ©2005 Robert J. Lillie East Pacific Rise Mid-Atlantic Ridge A  Continental Rift  can be Viewed as the On-land Continuation of a  Mid-Ocean Ridge Introduction to Geophysics-KFUPM
Parks and Plates ©2005 Robert J. Lillie Basin and Range Province East Pacific Rise Mid-Atlantic Ridge Gulf of California A  Continental Rift  can be Viewed as the On-land Continuation of a  Mid-Ocean Ridge Introduction to Geophysics-KFUPM
Parks and Plates ©2005 Robert J. Lillie Active Continental Rifts Death Valley Salton Sea Introduction to Geophysics-KFUPM National Park Lands
Moho DEPTH relate to tectonic history? Introduction to Geophysics-KFUPM Fig.4.17 of Lillie
Introduction to Geophysics-KFUPM Fig 4.18 of Lillie
Formation of Oceanic Crust Introduction to Geophysics-KFUPM Parks and Plates ©2005 Robert J. Lillie
DIVERGENT PLATE BOUNDARY DEVELOPMENT Introduction to Geophysics-KFUPM Parks and Plates ©2005 Robert J. Lillie
Ocean/Continent Subduction Zone Introduction to Geophysics-KFUPM Parks and Plates ©2005 Robert J. Lillie
Introduction to Geophysics-KFUPM Fig 4.19 of Lillie
Continental Rifting  eventually open an  Ocean Basin Parks and Plates ©2005 Robert J. Lillie Introduction to Geophysics-KFUPM
CONVERGENT PLATE BOUNDARY Subduction Zone Introduction to Geophysics-KFUPM Parks and Plates ©2005 Robert J. Lillie Accretionary Wedge Volcanic Arc
CONVERGENT PLATE BOUNDARY Continental Collision Introduction to Geophysics-KFUPM Parks and Plates ©2005 Robert J. Lillie
Problems 4-3, 4-5, 4-6, 4-7 Introduction to Geophysics-KFUPM Homework due to April 15

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ÖNCEL AKADEMİ: INTRODUCTION TO GEOPHYSICS

  • 1. Introduction to Geophysics Ali Oncel [email_address] Department of Earth Sciences KFUPM Tectonic Interpretation of Seismic Refraction Profiles Introduction to Geophysics-KFUPM
  • 2.
  • 3.
  • 4.
  • 5.
  • 6. Parks and Plates ©2005 Robert J. Lillie Plate Boundaries Introduction to Geophysics-KFUPM
  • 7. Introduction to Geophysics-KFUPM A. Jon Kimerling Parks and Plates ©2005 Robert J. Lillie Raised Relief Map of North America and Adjacent Oceans
  • 8. Introduction to Geophysics-KFUPM Due to shallow hot mantle Due to cold lithospheric plate Map of P-wave Velocity (km/s)
  • 9. Parks and Plates ©2005 Robert J. Lillie Active Continental Rifts Advanced Rifting (Lower Elevations) Early Rifting (Higher Elevations) Introduction to Geophysics-KFUPM National Park Lands
  • 10. Introduction to Geophysics-KFUPM Map of P-wave Velocity (km/s)
  • 11. Introduction to Geophysics-KFUPM Crustal thinning due to Continental rifting Remember that Red Sea is a good example for Continental Rifting. Map of Crustal Thickness (km)
  • 12. Parks and Plates ©2005 Robert J. Lillie Crustal Thinning at Continental Rifts Introduction to Geophysics-KFUPM As the lithosphere rips apart, the underlying asthenosphere becomes shallow while the crust still fairly thick. The buoyancy of the shallow asthenosphere and thick crust results in high overall elevation of the Basin.
  • 13. Crustal Thinning at Continental Rifts Parks and Plates ©2005 Robert J. Lillie Grand Teton National Park, Wyoming Great Basin National Park, Nevada Introduction to Geophysics-KFUPM
  • 14. Crustal Thinning at Continental Rifts Parks and Plates ©2005 Robert J. Lillie Introduction to Geophysics-KFUPM As the continental crust thins, it is less buoyant. Elevations are lower through the region.
  • 15. Parks and Plates ©2005 Robert J. Lillie Sagauro National Park, Arizona Death Valley National Park, California Crustal Thinning at Continental Rifts Introduction to Geophysics-KFUPM
  • 16. Parks and Plates ©2005 Robert J. Lillie Crustal Thinning at Continental Rifts Introduction to Geophysics-KFUPM
  • 17. Parks and Plates ©2005 Robert J. Lillie Salton Sea Gulf of California Crustal Thinning at Continental Rifts Introduction to Geophysics-KFUPM
  • 18. Continental Rifting eventually open an Ocean Basin Parks and Plates ©2005 Robert J. Lillie Introduction to Geophysics-KFUPM Red Sea is a good example for Continental Rifting (see pp. 50, Lillie 2005).
  • 19. Parks and Plates ©2005 Robert J. Lillie Continental Rifting eventually open an Ocean Basin Introduction to Geophysics-KFUPM
  • 20. Parks and Plates ©2005 Robert J. Lillie Continental Rifting eventually open an Ocean Basin Introduction to Geophysics-KFUPM
  • 21. Parks and Plates ©2005 Robert J. Lillie East Pacific Rise Mid-Atlantic Ridge A Continental Rift can be Viewed as the On-land Continuation of a Mid-Ocean Ridge Introduction to Geophysics-KFUPM
  • 22. Parks and Plates ©2005 Robert J. Lillie Basin and Range Province East Pacific Rise Mid-Atlantic Ridge Gulf of California A Continental Rift can be Viewed as the On-land Continuation of a Mid-Ocean Ridge Introduction to Geophysics-KFUPM
  • 23. Parks and Plates ©2005 Robert J. Lillie Active Continental Rifts Death Valley Salton Sea Introduction to Geophysics-KFUPM National Park Lands
  • 24. Moho DEPTH relate to tectonic history? Introduction to Geophysics-KFUPM Fig.4.17 of Lillie
  • 25. Introduction to Geophysics-KFUPM Fig 4.18 of Lillie
  • 26. Formation of Oceanic Crust Introduction to Geophysics-KFUPM Parks and Plates ©2005 Robert J. Lillie
  • 27. DIVERGENT PLATE BOUNDARY DEVELOPMENT Introduction to Geophysics-KFUPM Parks and Plates ©2005 Robert J. Lillie
  • 28. Ocean/Continent Subduction Zone Introduction to Geophysics-KFUPM Parks and Plates ©2005 Robert J. Lillie
  • 29. Introduction to Geophysics-KFUPM Fig 4.19 of Lillie
  • 30. Continental Rifting eventually open an Ocean Basin Parks and Plates ©2005 Robert J. Lillie Introduction to Geophysics-KFUPM
  • 31. CONVERGENT PLATE BOUNDARY Subduction Zone Introduction to Geophysics-KFUPM Parks and Plates ©2005 Robert J. Lillie Accretionary Wedge Volcanic Arc
  • 32. CONVERGENT PLATE BOUNDARY Continental Collision Introduction to Geophysics-KFUPM Parks and Plates ©2005 Robert J. Lillie
  • 33. Problems 4-3, 4-5, 4-6, 4-7 Introduction to Geophysics-KFUPM Homework due to April 15

Notas del editor

  1. qqq
  2. What is the reason that makes mantle hot?
  3. We have discussed so far how velocity is changed based upon the temperature changes due to tectonics.