A mechanism for crustal thinning without lateral extension
- 7 December 1990
- journal article
- Published by American Geophysical Union (AGU) in Geophysical Research Letters
- Vol. 17 (13) , 2417-2420
- https://doi.org/10.1029/gl017i013p02417
Abstract
No abstract availableThis publication has 10 references indexed in Scilit:
- The influence of second-scale convection on the thickness of continental lithosphere and crustTectonophysics, 1991
- Two-dimensional inverse modeling of crustal thermal regime with application to East European geotraversesJournal of Geophysical Research, 1990
- Topography and Geoid Undulations Caused By Small-Scale Convection Beneath Continental Lithosphere of Variable Elastic ThicknessGeophysical Journal International, 1989
- Correction to “Rheology of the lithosphere: Selected topics”Reviews of Geophysics, 1987
- Structural model of the subcrustal lithosphere in central EuropePublished by Wiley ,1987
- Estimation of crustal viscosities and shear stresses from an extrapolation of experimental steady state flow dataPublished by Wiley ,1987
- Steady state, secondary convection beneath lithospheric plates with temperature‐ and pressure‐dependent viscosityJournal of Geophysical Research, 1984
- Mechanism of continental crust subsidence in the Alpine BeltTectonophysics, 1984
- Evolution of the Pannonian Basin System: 2. Subsidence and thermal historyTectonics, 1983
- The mechanisms of creep in olivinePhilosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences, 1978