Subsidence of "normal" seafloor: Observations do indicate "flattening"
Seafloor topography is a key observational constraint upon the evolution of the oceanic lithosphere. Specifically, plots of oceanic depth (z) versus crustal age (t) for “normal” seafloor are well explained by depth-age predictions of thermal contraction models such as the half-space and cooling plat...
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| Format: | Default Article |
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2010
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| Online Access: | https://hdl.handle.net/2134/13011 |
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