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Stresses in rock outside buckled layers
International Journal of Rock Mechanics and Mining Sciences & Geomechanics Abstracts, 1979Abstract The author presents a theory of folding stresses in rocks, based on assumption of elastic equilibrium or slow viscous flow and a known fold geometry. The theory was first formulated in 1960–1961 and applied in practical problems. At this stage the general form of the solution is derived, applicable to arbitrary fold configurations.
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Glacial Erosion in Tilted Rock Layers
The Journal of Geology, 1955Isle Royale in Lake Superior and the Rove area of northeastern Minnesota have valley and ridge topographies controlled by bands of massive, poorly jointed rock, alternating with highly jointed rock units. The ridges are asymmetrical in cross section, with gentle dip slopes on one side and precipitous antidip slopes on the other.
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Model studies of folding rock layers.
1972This item was digitized as part of a project to share McGill's intellectual legacy with the public. If you are the copyright holder or a relative of the copyright holder who is deceased, you may request withdrawal by emailing escholarship.library@mcgill.ca.
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Numerical investigation of hydraulic fracture height growth in layered rock based on peridynamics
Theoretical and Applied Fracture Mechanics, 2023Diansen Yang
exaly
Textural Equilibrium in Layered Igneous Rocks
1987Rocks of many layered intrusions, adcumulate rocks in particular, are in local textural equilibrium; the shape and contiguity of grains are controlled by surface energies. Existing cumulus theory takes no account of the effects of surface energy in determining the textures which form in layered intrusions.
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Hydraulic fracturing model of a layered rock mass based on peridynamics
Engineering Fracture Mechanics, 2021Diansen Yang +2 more
exaly