An improved estimate of lithospheric thickness based on a reinterpretation of tilt data from Pleistocene Lake Algonquin
A reinterpretation of relative-uplift data associated with the deformed strandline of Pleistocene Lake Algonquin is presented. The new analysis is based on a dynamic model that allows for the finite rate of retreat of the Laurentide ice sheet and the viscous relaxation of the Earth's mantle. At...
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| Format: | Article in Journal/Newspaper |
| Language: | English |
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1985
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| Online Access: | https://doi.org/10.18419/opus-7127 http://nbn-resolving.de/urn:nbn:de:bsz:93-opus-50794 http://elib.uni-stuttgart.de/handle/11682/7144 |