Our analysis shows that the only viable mechanism able to explain the uplift is crustal thickening by basal intrusions, suggesting that intrusive processes play a significant role even on islands ...

The vertical exaggeration is 3:1. The integrated interpretation of seismic reflection data and seismic velocity models shows significant along-strike differences in the number of fault splays and the ...

In one location, the accumulated land uplift has reached about 3 centimeters ... the seismic source areas since the onset of the crustal deformation. That indicates something has gathered there ...

The latter references the uplift of land and crustal deformation in response to the loss of ice sheet mass loading as they ...