Abstract
10) the lithosphere is unable to sustain appreciable crustal elevation contrasts. The results of these numerical experiments show that systems in which the effective viscosities are such that the maximum deviatoric stresses are between 1 kbar Copyright © 1982, Wiley Blackwell. All rights reserved
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APA
England, P., & McKenzie, D. (1982). A thin viscous sheet model for continental deformation. Geophysical Journal of the Royal Astronomical Society, 70(2), 295–321. https://doi.org/10.1111/j.1365-246X.1982.tb04969.x
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