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Superposition of compaction and plane strain

Superposition of compaction and plane strain
Superposition of compaction and plane strain
The coaxial and non-coaxial superposition of tectonic (biaxial or plane) strain on compactional (uniaxial) strain is examined and total finite strains and deformation paths calculated. Both prolate and oblate strains may result, depending on the relative orientations of the two strains. The implications of superposed strain are discussed in relation to naturally occurring strains in rocks, and various patterns of finite strain and deformation fields recognized.

0040-1951
35-54
Sanderson, David J.
5653bc11-b905-4985-8c16-c655b2170ba9
Sanderson, David J.
5653bc11-b905-4985-8c16-c655b2170ba9

Sanderson, David J. (1976) Superposition of compaction and plane strain. Tectonophysics, 30 (1-2), 35-54. (doi:10.1016/0040-1951(76)90136-0).

Record type: Article

Abstract

The coaxial and non-coaxial superposition of tectonic (biaxial or plane) strain on compactional (uniaxial) strain is examined and total finite strains and deformation paths calculated. Both prolate and oblate strains may result, depending on the relative orientations of the two strains. The implications of superposed strain are discussed in relation to naturally occurring strains in rocks, and various patterns of finite strain and deformation fields recognized.

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Published date: January 1976

Identifiers

Local EPrints ID: 73785
URI: http://eprints.soton.ac.uk/id/eprint/73785
DOI: doi:10.1016/0040-1951(76)90136-0
ISSN: 0040-1951
PURE UUID: a0e6cb89-5ea7-4aea-93e6-c8fca3f0d7e9
ORCID for David J. Sanderson: ORCID iD orcid.org/0000-0002-2144-3527

Catalogue record

Date deposited: 11 Mar 2010
Last modified: 14 Mar 2024 02:53

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Author: David J. Sanderson ORCID iD

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