State of stress and crustal deformation along weak transform faults

Saved in:
Authors:Zoback, Mark D.
Author Affiliations:Primary:
Stanford Univ., Dep. Geophys., Stanford, CA, United States
Other:
Univ. Durham, United Kingdom
Univ. Liverpool, United Kingdom
Volume Title:Tectonic stress in the lithosphere
Volume Authors:Whitmarsh, R. B., editor; Bott, M. H. P.; Fairhead, J. D.; Kusznir, N. J.
Source:Philosophical Transactions of the Royal Society of London, Series A: Mathematical and Physical Sciences, 337(1645), p.141-150; A Royal Society discussion meeting ; Tectonic stress in the lithosphere, London, United Kingdom, Apr. 10-11, 1991, edited by R. B. Whitmarsh, M. H. P. Bott, J. D. Fairhead and N. J. Kusznir. Publisher: Royal Society of London, London, United Kingdom. ISSN: 0080-4614
Publication Date:1991
Note:In English. 41 refs.; illus. incl. sect., sketch map
Summary:While the frictional strength of the upper crust is high, the frictional resistance to motion along transform plate boundaries is very low. The horizontal principal stresses must therefore be orientated [vertical bar][vertical bar] and perpendicular the transform-fault zone to minimize shear stresses acting [vertical bar][vertical bar] the transform. Near-fault normal compression and fault-normal crustal shortening is expected along plate margins accommodating relative convergence (transgressive margins). Along transtensional margins extension is expected to occur perpendicular the transform. [R.K.H.]
Subjects:Crust; Faults; Plate boundaries; Processes; Stress; Strike-slip faults; Transform faults
Abstract Numbers:92M/2333
Record ID:1992003419
Copyright Information:GeoRef, Copyright 2019 American Geosciences Institute. Reference includes data from Mineralogical Abstracts, United Kingdom, Twickenham, United Kingdom
Tags: Add Tag
No Tags, Be the first to tag this record!
Be the first to leave a comment!
You must be logged in first