The influence of second-scale convection on the thickness of continental lithosphere and crust
Authors:
- Harro SchmelingHSHarro Schmeling
- Gabriele MarquartGMGabriele Marquart
- 1 April 1991
- journal article
- research article
- Published by Elsevier in Tectonophysics
- Vol. 189 (1-4) , 281-306
Abstract
No abstract availableThis publication has 56 references indexed in Scilit:
- A benchmark comparison for mantle convection codesGeophysical Journal International, 1989
- Thermally induced phase changes, lateral heterogeneity of the mantle, continental roots, and deep slab anomaliesJournal of Geophysical Research, 1987
- Analysis of the cooling of a variable-viscosity fluid with applications to the EarthGeophysical Journal International, 1987
- Deep structure of the European-Mediterranean area from seismological dataTectonophysics, 1985
- Mechanism of continental crust subsidence in the Alpine BeltTectonophysics, 1984
- Convection with pressure- and temperature-dependent non-Newtonian rheologyGeophysical Journal International, 1984
- Convection in a variable-viscosity fluid: Newtonian versus power-law rheologyEarth and Planetary Science Letters, 1983
- Shear modulus and Q of forsterite and dunite near partial melting from forced-oscillation experimentsPhysics of the Earth and Planetary Interiors, 1982
- Limits on lithospheric stress imposed by laboratory experimentsJournal of Geophysical Research, 1980
- The Strength of the Earth's CrustThe Journal of Geology, 1914