The relationship between principal stress directions and the geometry of kinks in foliated rocks-Reference-Cited by-同舟云学术

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The relationship between principal stress directions and the geometry of kinks in foliated rocks

Published:1974-02 Issue:3 Volume:21 Page:287-300
ISSN:0040-1951
Container-title:Tectonophysics
language:en
Short-container-title:Tectonophysics

Author:

Gay N.C.,Weiss L.E.

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geophysics

Reference18 articles.

1. The geometry of a natural orthorhombic system of kink bands;Anderson,1968

2. Kink band development in the Lake St. Joseph area, Northwestern Ontario;Clifford,1968

3. Development of internal structures in deformed anisotropic rocks;Cobbold;Tectonophysics,1971

4. The origin and development of kink-bands in a foliated body;Dewey;Geol. J.,1969

5. Experimental study of kinkband development in Martinsburg slate;Donath,1968

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1. Kink-bands as indicators of shock-wave propagation direction: Results from experimental impact cratering on gneiss;Journal of Structural Geology;2024-03

2. Kinematic and tectonic implications of crenulation cleavage, kink bands, and mesoscopic folds in the Baraboo Syncline, Wisconsin (∼1.45 Ga Picuris Orogen);Journal of Structural Geology;2024-01

3. Deformation trail tracking in S-tectonites of the Darjeeling-Sikkim Himalaya: The kink band perspective;Journal of Asian Earth Sciences;2023-10

4. Accommodation structures during kink band evolution; quantitative methods applied to Late Variscan deformation of Portugal;Journal of Structural Geology;2022-03

5. Stress, microstructure, and deformation mechanisms during subduction underplating at the depth of tremor and slow slip, Franciscan Complex, northern California;Journal of Structural Geology;2022-01

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