1988
DOI: 10.1007/bf01019673
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Gravity-induced stresses in stratified rock masses

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Cited by 47 publications
(25 citation statements)
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“…They also depend on how the rock mass properties and the degree of anisotropy vary with depth. The effect of such variations on gravity-induced stresses has already been discussed by Amadei and Savage [7] and Amadei et al [2] for horizontally regularly jointed and layered rock masses. The solution presented in this paper can also be used to predict stresses in rock masses for which the deformability properties vary with depth only.…”
Section: Resultsmentioning
confidence: 73%
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“…They also depend on how the rock mass properties and the degree of anisotropy vary with depth. The effect of such variations on gravity-induced stresses has already been discussed by Amadei and Savage [7] and Amadei et al [2] for horizontally regularly jointed and layered rock masses. The solution presented in this paper can also be used to predict stresses in rock masses for which the deformability properties vary with depth only.…”
Section: Resultsmentioning
confidence: 73%
“…The other three stress components o~, oy and ~y can be obtained by substituting the conditions %~ =Ty: = 0 and o: = pgz into equation (2). This results in the following system of three equations:…”
Section: (5)mentioning
confidence: 99%
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“…Both the soil and the stratified rock masses show the nature of anisotropy. For this reason, theoretical or numerical models should be able to simulate this kind of layered soils and rocks as cross-anisotropic medium (Amadei et al, 1988;Barden, 1963;Gibson, 1974;Lee & Yang, 1998;Sekowski, 1986;Sheorey, 1994). In this paper, the soil mass is modelled as a linearly elastic medium with cross-anisotropic properties.…”
Section: Introductionmentioning
confidence: 99%