Hostname: page-component-586b7cd67f-gb8f7 Total loading time: 0 Render date: 2024-11-27T21:21:08.142Z Has data issue: false hasContentIssue false
  • English
  • Français

Regional Study of Epidote, Mica, and Albite Fabrics of the Moines

Published online by Cambridge University Press:  01 May 2009

C. B. Crampton
C. B. Crampton
Affiliation:
30 Mount Preston, Leeds, 2.
Get access Rights & Permissions [Opens in a new window]

Abstract

The great majority of Moine lineations are mica structures, and together with a parallel preferred orientation of epidote [010]-axes, are directed mainly into the south-east quadrant. This orientation is retained within the crush zone alongside the Moine Thrust. The regional preferred orientation of muscovite [100]-axes and [001]-axes is consistent with north-east and south-west movements except within the crush zone where fabric reorientation suggests movements normal to this direction. The growth of albite textures and fabric is intimately associated with thrust plane movements, the preferred orientation of albite suggesting a south-east and north-west vertical plane of deformation.

Type
Articles
Information
Geological Magazine , Volume 94 , Issue 2 , April 1957 , pp. 89 - 103
Copyright
Copyright © Cambridge University Press 1957

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

REFERENCES

Berek, M., 1924. Universaldrehtischmethoden. Borntraeger, Berlin.Google Scholar
Ingerson, E., 1936. Fabric Analysis of a Coarsely Crystalline Polymeta-morphic Tectonite. Amer. Journ. Sci., xxxi, 161–187.CrossRefGoogle Scholar
Kvale, A., 1935. Linear structures and their relation to movement in the Caledonides of Scandinavia and Scotland. Quart. Journ. Geol. Soc., cix, 51–73.Google Scholar
Ladurner, J., 1951. Deformation, Wachstum und Regelung der Epidote als Gefügekorn und Einkristall. Neues Jahrb. Abh., lxxxii, 317–412.Google Scholar
Larsen, E. S., and Bridgman, P. W., 1938. Shearing Experiments on some selected minerals and mineral combinations. Amer. Journ. Sci., xxxvi, 81–94.CrossRefGoogle Scholar
Mügge, O., 1898. Ueber Translation under verwandte Erscheinungen in Kristallen. Neues Jahrb. Min. Geol., i, 71–158.Google Scholar
Osborn, E. F., 1939. Petrology of Val Verde Tonalite. Bull. Geol. Soc. Amer., 1, 921–950.CrossRefGoogle Scholar
Phillips, F. C., 1937. A fabric study of some Moine Schists and associated rocks. Quart. Journ. Geol. Soc., xciii, 581–620.CrossRefGoogle Scholar
Phillips, F. C., 1945. The micro-fabric of the Moine Schists. Geol. Mag., lxxxii, 205–220.CrossRefGoogle Scholar
Sander, B., 1930. Gefügekunde der Gestine. Springer, Vienna.CrossRefGoogle Scholar
Sander, B., 1950. Einführung in die Gefügekunde der Geologischen Korper. Part 1. Springer, Vienna.CrossRefGoogle Scholar
Schmidt, W., 1928. Zur Regelung zweiachsiger Mineralien in kristallinen Schiefern. Neues Jahrb. Min. etc., lvii A, 203–222.Google Scholar
Turner, F. J., and Hutton, C. O., 1940. Some porphyroblastic albite schists from Waikovaiti River, Otago. Trans. Roy. Soc. N.Z., lxxi, 223–240.Google Scholar
Wenk, E., 1936. Zur Genese der Bandergneise von Orno Huvud. Bull. Geol. Inst. Upsala, xxvi, 53–89.Google Scholar