| Literature DB >> 17821590 |
Abstract
Recent information from experimentally deformed dunite coupled with a reanalysis of data on the Fennoscandian postglacial rebound suggest that the rheological behavior of the upper mantle is distinctly non-Newtonian, and that the shear strain rate is proportional to the shear stress raised to about the third power.Year: 1973 PMID: 17821590 DOI: 10.1126/science.181.4106.1242
Source DB: PubMed Journal: Science ISSN: 0036-8075 Impact factor: 47.728