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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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書(shū)目名稱(chēng)Glacial Isostasy, Sea-Level and Mantle Rheology
編輯R. Sabadini,K. Lambeck,E. Boschi
視頻videohttp://file.papertrans.cn/386/385810/385810.mp4
叢書(shū)名稱(chēng)Nato Science Series C:
圖書(shū)封面Titlebook: Glacial Isostasy, Sea-Level and Mantle Rheology; R. Sabadini,K. Lambeck,E. Boschi Book 1991 Springer Science+Business Media Dordrecht 1991
描述by K. Lambeck, R. Sabadini and E. B08Chi Viscosity is one of the important material properties of the Earth, controlling tectonic and dynamic processes such as mantle convection, isostasy, and glacial rebound. Yet it remains a poorly resolved parameter and basic questions such as whether the planet‘s response to loading is linear or non-linear, or what are its depth and lateral variations remain uncertain. Part of the answer to such questions lies in laboratory observations of the rheology of terrestrial materials. But the extrapolation of such measurements from the laboratory environment to the geological environment is a hazardous and vexing undertaking, for neither the time scales nor the strain rates characterizing the geological processes can be reproduced in the laboratory. General rules for this extrapolation are that if deformation is observed in the laboratory at a particular temperature, deformation in geological environments will occur at a much reduced temperature, and thatif at laboratory strain rates a particular deformation mechanism dominates over all others, the relative importance of possible mechanisms may be quite different at the geologically encountered strain
出版日期Book 1991
關(guān)鍵詞Climatology; Europe; Greenhouse gas; Holoz?n; Isostasy; Northeaster; Pleistocene; Scale; Tide; fault; hydrogeo
版次1
doihttps://doi.org/10.1007/978-94-011-3374-6
isbn_softcover978-94-010-5492-8
isbn_ebook978-94-011-3374-6Series ISSN 1389-2185
issn_series 1389-2185
copyrightSpringer Science+Business Media Dordrecht 1991
The information of publication is updating

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Late Pleistocene and Holocene Sea-Level Change; Evidence for Lateral Mantle Viscosity Structure?esponse occurs and that effective upper mantle viscosities may range through an order of magnitude. Highest values occur beneath the Canadian Shield and lowest values beneath the Pacific Islands. The results are largely consistent with the evidence for lateral variation in seismic shear-wave velocities.
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978-94-010-5492-8Springer Science+Business Media Dordrecht 1991
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G. S. Bajpai,Garima Pal,Advait TambeSignificant case studies of regional sea-level changes during the Holocene, extracted from part of a broader study, are considered. Some of them are compared to predictions obtained by global isostatic models.
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發(fā)表于 2025-3-22 14:31:56 | 只看該作者
A Survey of Relative Sea-Level Changes Observed During the HoloceneSignificant case studies of regional sea-level changes during the Holocene, extracted from part of a broader study, are considered. Some of them are compared to predictions obtained by global isostatic models.
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發(fā)表于 2025-3-22 19:02:06 | 只看該作者
https://doi.org/10.1007/978-94-011-3374-6Climatology; Europe; Greenhouse gas; Holoz?n; Isostasy; Northeaster; Pleistocene; Scale; Tide; fault; hydrogeo
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發(fā)表于 2025-3-23 00:16:52 | 只看該作者
A model for Devensian and Flandrian glacial rebound and sea-level change in Scotlandth the minimum reconstruction proposed by Boulton et al. (1985). In particular, a major ice sheet could not have existed over the North Sea much after about 23 000 a BP. Also, the ice sheet was less extensive over the continental shelf west of Scotland than assumed in these maximum reconstruction mo
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