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Titlebook: Glacial Isostasy, Sea-Level and Mantle Rheology; R. Sabadini,K. Lambeck,E. Boschi Book 1991 Springer Science+Business Media Dordrecht 1991

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https://doi.org/10.1007/978-94-015-6853-1scosity increases beneath continental regions with respect to oceanic regions may be able to explain the systematically lower viscosity values inferred from sea-level data from Pacific Island sites. Our findings are potentially very important in the interpretation of GPS data.
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Generic Linear Recurrence Sequences,0 to 0 m aht, a rapid rise to ca. 34 m aht by ca. 8.4 ka, and then a final interval of emergence. Although supported by several lines of evidence this scenario is still a hypothesis, but it may indicate that short-lived glacial re-advances can result in an appreciable depression of the crust at sites proximal to the ice margin.
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Deep Continental Roots: The Effects of Lateral Variations of Viscosity on Post-Glacial Reboundscosity increases beneath continental regions with respect to oceanic regions may be able to explain the systematically lower viscosity values inferred from sea-level data from Pacific Island sites. Our findings are potentially very important in the interpretation of GPS data.
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The Study of Inferred Patterns of Holocene Sea-Level Change from Atlantic and Other European Coastalrm tectonic influences. The work here reviews the uplift and subsidence data available from the region and discusses the subsequent modelling of earth rheology and the present thrust of approaches here to sea-level studies.
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