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Ali Oncel [email_address] Department of Earth Sciences KFUPM Gravity and Isostasy Introduction to Geophysics Introduction to Geophysics-KFUPM
Previous Lecture ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],Introduction to Geophysics-KFUPM
Parks and Plates,pp.27 ©2005 Robert J. Lillie Introduction to Geophysics-KFUPM
Parks and Plates ©2005 Robert J. Lillie
Parks and Plates ©2005 Robert J. Lillie Introduction to Geophysics-KFUPM
http://www.moorlandschool.co.uk/earth/tectonic.htm Introduction to Geophysics-KFUPM
Parks and Plates ©2005 Robert J. Lillie Topography of the Ocean Floor Introduction to Geophysics-KFUPM ©1977, Marie Thorpe
National Aeronautics and Space Administration  Two Forms of Isostatic Uplift pp.28 Parks and Plates  ©2005 Robert J. Lillie Introduction to Geophysics-KFUPM Low density due to higher temperature
http://www.moorlandschool.co.uk/earth/tectonic.htm Two Forms of Isostatic Uplift Introduction to Geophysics-KFUPM
What is Isostatic Equilibrium?   ,[object Object],[object Object],[object Object],[object Object],[object Object],Introduction to Geophysics-KFUPM
Bouguer Anomaly ,[object Object],[object Object],Why? ,[object Object],Introduction to Geophysics-KFUPM 2.67 g/cm 3 3.3 g/cm 3 Mantle http://www.moorlandschool.co.uk/earth/tectonic.htm
Example from Arabia Introduction to Geophysics-KFUPM
Example from Arabia Data Source: Cornell University ,[object Object],[object Object],[object Object],Introduction to Geophysics-KFUPM
Homework, Due to May 17 ,[object Object],[object Object],[object Object],Introduction to Geophysics-KFUPM
The quiz of the week For the following equation, define the variables: FAA= g obs  – g th  +FAC BA = FAA – BC + TC Introduction to Geophysics-KFUPM

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