FLOW AND STRAIN PATTERNS AT THE TERMINATIONS OF TAPERED SHEAR ZONES

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dc.contributor.author Mandal N.
dc.contributor.author Samanta S.K.
dc.contributor.author Chakraborty C.
dc.date.accessioned 2021-04-12T06:59:37Z
dc.date.available 2021-04-12T06:59:37Z
dc.date.issued 2002
dc.identifier https://www.elibrary.ru/item.asp?id=827066
dc.identifier.citation Journal of Structural Geology, 2002, 24, 2, 297-309
dc.identifier.issn 0191-8141
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/27674
dc.description.abstract With the help of corner flow theory, this paper numerically analyzes the deformation pattern at the terminations of tapered shear zones, the walls of which are rigid and move parallel to each other in opposite directions. The overall flow pattern is characterized by curvilinear particle paths that show convexity towards and opposite to the tapering direction respectively for low (<5°) and high (>10°) inclinations of the wall verging opposite to the sense of wall movement. In tapered shear zones there are two distinct fields of instantaneous shortening and extension parallel to the direction of wall movement. Numerical models reveal that the finite strain distributions are generally asymmetrical with larger strain concentration occurring near the wall verging opposite to sense of wall movement. The S-foliation trajectories show a curvilinear pattern, convexing against the tapering direction. The analysis of rotationality (vorticity) indicates that the sense of vorticity near the synthetically verging wall is reverse to the sense of wall movement; however Wk is one everywhere within the shear zone.
dc.subject NON-PARALLEL WALLS
dc.subject SIMPLE SHEAR
dc.subject DUCTILE FLOW
dc.subject VORTICITY
dc.subject FOLIATION
dc.title FLOW AND STRAIN PATTERNS AT THE TERMINATIONS OF TAPERED SHEAR ZONES
dc.type Статья


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