Hostname: page-component-848d4c4894-5nwft Total loading time: 0 Render date: 2024-05-18T03:10:16.058Z Has data issue: false hasContentIssue false
  • English
  • Français

Angle Between the Principal Horizontal Stress and Transcurrent Faults

Published online by Cambridge University Press:  01 May 2009

H. W. Wellman
H. W. Wellman
Affiliation:
Geological Survey, 156 The Terrace, Wellington C. 1, New Zealand.
Rights & Permissions [Opens in a new window]

Abstract

An abstract is not available for this content so a preview has been provided. As you have access to this content, a full PDF is available via the ‘Save PDF’ action button.
Image of the first page of this content. For PDF version, please use the ‘Save PDF’ preceeding this image.'
Type
Correspondence
Information
Geological Magazine , Volume 91 , Issue 5 , October 1954 , pp. 407 - 408
Copyright
Copyright © Cambridge University Press 1954

References

REFERENCES

Anderson, J. G. C., 1942. The Dynamics of Faulting. Edinburgh.Google Scholar
Auden, J. B., 1954. Erosional Patterns and Fracture Zones in Peninsular India. Geol. Mag., xci, 116–128.Google Scholar
Leedal, G. P., and Walker, G. P. L., 1954. Tear Faults in the Barnesmore area, Donegal. Geol. Mag., xci, 116–128.CrossRefGoogle Scholar
Hill, M. L., and Dibblee, T. W., 1953. San Andreas, Garlock, and Big Pine Faults, California. Bull. Geol. Soc. Amer., lxiv, 443–458.CrossRefGoogle Scholar
Wellman, H. W., 1953. Data for the study of Recent and late Pleistocene Faulting in the South Island of New Zealand. N.Z. Journ. Sci. & Tech., B, 34 (4), 271–288.Google Scholar