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GEOREF RECORD

Evidence for flexural shear folding associated with extensional faults

W. G. Higgs, G. D. Williams and C. M. Powell
Evidence for flexural shear folding associated with extensional faults
Geological Society of America Bulletin (May 1991) 103 (5): 710-717

Abstract

The maintainance of bed length and bed thickness within the hanging wall of extensional fault systems requires the development of bed-parallel shear. Four field examples of bed-parallel-shear related structures are described from a number of positions within the hanging wall and footwall to extensional faults. Flexural shear folding is a characteristic of both fault bend and fault-propagation folding. The dominant direction of the over-riding shear is directed toward the fault surface in the case of fault-bend folds. The fault surface may be considered to represent the finite neutral surface of the fold. In extensional fault-propagation folds, the direction of the overriding shear is toward the synclinalfold axial surface. The observations suggest that the direction of flexural shear for extensional and contractional folds is opposite for folds of geometrically similar form.


ISSN: 0016-7606
EISSN: 1943-2674
Coden: BUGMAF
Serial Title: Geological Society of America Bulletin
Serial Volume: 103
Serial Issue: 5
Title: Evidence for flexural shear folding associated with extensional faults
Affiliation: Univ. Keele, Dep. Geol., Keele, United Kingdom
Pages: 710-717
Published: 199105
Text Language: English
Publisher: Geological Society of America (GSA), Boulder, CO, United States
References: 17
Accession Number: 1991-020008
Categories: Structural geology
Document Type: Serial
Bibliographic Level: Analytic
Illustration Description: illus. incl. sects.
Country of Publication: United States
Secondary Affiliation: GeoRef, Copyright 2019, American Geosciences Institute.
Update Code: 1991
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