1950
DOI: 10.1130/0016-7606(1950)61[509:csoeet]2.0.co;2
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Conjugate Sets of en Echelon Tension Fractures in the Athens Limestone at Riverton, Virginia

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Cited by 42 publications
(10 citation statements)
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“…2). Beach (1975), drawing on prior work by Shainin (1950) and Riedel (1929), proposed a kinematic model in which Mode I fractures developing within an existing shear zone become progressively rotated by simple shear, while their tips continue to propagate parallel with the maximum compressive stress axis, and hence develop a sigmoidal geometry (Fig. 2a).…”
Section: Models Of Sigmoidal Vein Formationmentioning
confidence: 98%
“…2). Beach (1975), drawing on prior work by Shainin (1950) and Riedel (1929), proposed a kinematic model in which Mode I fractures developing within an existing shear zone become progressively rotated by simple shear, while their tips continue to propagate parallel with the maximum compressive stress axis, and hence develop a sigmoidal geometry (Fig. 2a).…”
Section: Models Of Sigmoidal Vein Formationmentioning
confidence: 98%
“…Although it is unlikely that Z1 bands initiate as purely tensional features, the following discussion of Z1 bands possibly nucleating as tension fractures is included due to the geometric similarly of PRZs and tension fracture arrays composed of sigmoidal gash fractures (e.g. Shainin 1950, Plates 1-2). Please note that the alternative interpretation may also apply to 12 bands.…”
Section: Z1 Band Nucleationmentioning
confidence: 99%
“…The movement picture is corroborated by the orientation of the fractures (for example, see Shainin, 1950). The cleavage is perpendicular to the last-formed part of the tension crack, thus also perpendicular to maximum compressive stress.…”
Section: Quarry (27)mentioning
confidence: 75%