The Mohorovicic discontinuity is a change in seismic wave velocity that is believed to take place because
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The Mohorovicic discontinuity is a change in seismic wave velocity that is believed to take place because of
a. structural changes in minerals of the same composition.
b. changes in the composition on both sides of the boundary.
c. a shift in the density of minerals of the same composition.
d. changes in the temperature with depth.
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