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- W2077303412 abstract "After introductory comments on scale-model theory, descriptions and discussions of experimental models of continental drift and orogenesis are presented. The driving mechanism of the models is the spontaneous overturn in layered systems with gravitationally unstable density stratification. The pattern of the overturn movement is similar to thermal convection currents. A model Pangaea breaks in tension above the upwelling branches of the overturn cells in the model mantle, and the fragments are set adrift by the horizontal limbs of the current. Though buckling occurs along the leading edges of the wandering continental fragments, this fold structure is not of the kind encountered in natural orogens. The latter kind of structures — including basement upheaval, batholith intrusion, nappe formation etc. — is generated in models with no net horizontal shortening across the orogen." @default.
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- W2077303412 date "1973-09-01" @default.
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- W2077303412 title "Experimental geodynamical models relating to continental drift and orogenesis" @default.
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