Dynamics of Long-Term Sea-Level Change and Vertical Motion of Continents
We formulate and apply dynamic models to better understand mantle processes and evolution, the vertical motion of continents, and regional and global sea-level change since 100 Ma. We show that evolving mid-to-upper mantle upwellings explain observed anomalously shallow bathymetry, the negative geoi...
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Format: | Thesis |
Language: | English |
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California Institute of Technology
2011
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Online Access: | https://dx.doi.org/10.7907/c7pg-qn55 https://resolver.caltech.edu/CaltechTHESIS:12012010-122030085 |