Hostname: page-component-586b7cd67f-tf8b9 Total loading time: 0 Render date: 2024-11-22T00:29:39.387Z Has data issue: false hasContentIssue false
  • English
  • Français

Tectonic transpression in Caledonian Spitsbergen

Published online by Cambridge University Press:  01 May 2009

W. B. Harland
W. B. Harland
Affiliation:
Department of Geology, Sedgwick Museum, Downing Street, Cambridge, CB2 3EQ
Get access Rights & Permissions [Opens in a new window]

Summary

In addition to the well-established extension, compression and transcurrent relative movements between plates of the lithosphere, this paper considers intermediate or oblique relative movements, namely, transtension and transpression. Transtension is already well established in oblique zones of ocean spreading which consist of stepped transform faults. Transpression is a more complex process. The tectonic consequences of a transpression model are outlined and it is suggested that the tectonic style in Caledonian Spitsbergen provides evidence for this transpression regime as an intermediate stage between compression and transcurrence. It is also suggested that transpression should occur generally and may relate the development of transcurrent faults in orogenic belts.

Type
Articles
Information
Geological Magazine , Volume 108 , Issue 1 , January 1971 , pp. 27 - 41
Copyright
Copyright © Cambridge University Press 1971

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Anderson, E. M. 1951. The Dynamics of Faulting and Dyke Formation with Applications to Britain. 2nd ed., Oliver & Boyd, Edinburgh.Google Scholar
Carey, S. W. 1958. A tectonic approach to continental drift; pp. 177–355 in Carey, S. W. (Ed.): Continental Drift, a Symposium. University of Tasmania, Hobart.Google Scholar
De Sitter, L. U. 1956. Structural Geology. 1st edn., 552 pp. McGraw-Hill Publishing Co. Ltd., London.Google Scholar
Dewey, John F. & Bird, John M. 1970. Mountain belts and the new global tectonics. J. geophys. Res. 75 (14), 2625–47.CrossRefGoogle Scholar
Gayer, R. A. 1969. The geology of the Femmilsjøen region of north-west Ny Friesland, Spitsbergen. Skr. norsk Polarinst. 145, 45 pp., 12 pls.Google Scholar
Harland, W. B. 1959. The Caledonian sequence in Ny Friesland, Spitsbergen. Q. Jl geol. Soc. Lond. 114, 307–42.CrossRefGoogle Scholar
Harland, W. B. 1961.An outline structural history of Spitsbergen, pp. 68–132 in Raasch, G. O. (Ed.): Geology of the Arctic, Vol. 1. University of Toronto Press (O.U.P.).Google Scholar
Harland, W. B. 1969.Contributions of Spitsbergen to understanding of tectonic evolution of North Atlantic region; pp. 817–51 in North Atlantic—Geology and Continental Drift, American Association of Petroleum Geologists, Memoir 12.Google Scholar
Harland, W. B. & Bayly, M. B. 1958. Tectonic regimes. Geol. Mag. 95, 89–104.CrossRefGoogle Scholar
Harland, W. B., Wallis, R. H. & Gayer, R. A. 1966. A revision of the Lower Hecla Hoek Succession in central North Spitsbergen and Correlation Elsewhere. Geol. Mag. 103 (1), 70–97.CrossRefGoogle Scholar
Holgate, N. 1969. Palaeozoic and Tertiary transcurrent movements on the Great Glen fault. Scott. J. Geol. 5, 97–139.CrossRefGoogle Scholar
Heezen, B. C. 1962. The deep sea floor. Chap. 9, pp. 235–288 in Runcorn, S. K. (Ed.): Continental Drift. Academic Press, New York and London.CrossRefGoogle Scholar
McConnell, R. B. 1969. The Association of granites with zones of stress and shearing. Bull. geol. Soc. Am. 80, 115–20.CrossRefGoogle Scholar
Moody, J. D. & Hill, M. J. 1956. Wrench fault tectonics. Bull. geol. Soc. Am. 67, 1207–46.CrossRefGoogle Scholar
Reitan, P. H. 1968. Frictional heat during metamorphism. Lithos 1, 151–63.CrossRefGoogle Scholar
Sutton, J. & Watson, J. 1959. Metamorphism in deep-seated zones of transcurrent movement at Kungwe Bay, Tanganyika Territory. J. Geol. 67, 1–13.CrossRefGoogle Scholar
Tromp, S. W. 1937. On the mechanism of the Geological Undulation Phenomena in general and of Folding in particular and their Application to the Problem of the ‘Roots of Mountains’ Theory, 184 pp. A. W. Sijthoff's Uitgeversmaatschappij N.V., Leiden.Google Scholar
Wilson, J. Tuzo. 1965. A new class of faults and their bearing on continental drift. Nature, Lond. 207, No. 4995, 343–7.CrossRefGoogle Scholar