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EARTH 135 Lecture Notes - Lecture 13: Center For Retrospective Digitization, Thermal Expansion, Multiple Integral
Change in ocean depth for cooling halfspace model. Test of the cooling halfspace model (section 4. 23 in ts) In this lecture, we are going to see a tesView Document
EARTH 135 Lecture Notes - Lecture 7: Bending, Boundary Value Problem, Bathymetry
Figure 1: figure 1: seamount loading. xp is the distance to the bulge. Lecture 7 : plate flexure due to a seamount: buoyancy: the equation for plate exView Document
EARTH 135 Lecture Notes - Lecture 6: Shear Stress, Shear Force
Summary : plate bending: the basic equation. D d4w dx4 = q(x) where d is the exural ridigity given by. 12(1 2) (1) (2) with h being the thickness of aView Document
EARTH 135 Lecture 4: Lecture4.1
When stress and strain are small, the relationship between them is linear. (1) stress has six independent components xx , yy , zz , xy , yz , zx with iView Document
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