Hostname: page-component-84b7d79bbc-l82ql Total loading time: 0 Render date: 2024-07-27T20:21:11.295Z Has data issue: false hasContentIssue false
  • English
  • Français

The Diorites and Associated Rocks of the Glen Tilt Complex

Published online by Cambridge University Press:  01 May 2009

W. A. Deer
W. A. Deer
Affiliation:
Department of Geology, The University, Manchester.
Get access Rights & Permissions [Opens in a new window]

Abstract

The diorites and Sron a' Chro' granite of the Glen Tilt complex enclose hornblende-schist xenoliths derived from the Dalradian epidiorites of the country rock. Small hornblendite xeoliths are found in the complex but are restricted to the diorite outcrop. Porphyroblastic hornblende is developed within the schist xenoliths and reaction zones rich in hornblende are formed around the xenoliths. The mineralogical and textural characteristics of these reaction products suggest that the typical two-hornblende generation appinites of the complex represent modified hornblende schist. A similar origin for the quartz-orthoclase-appinite of the complex is rejected and their development from hornblendite is indicated.

Type
Articles
Information
Geological Magazine , Volume 90 , Issue 1 , February 1953 , pp. 27 - 35
Copyright
Copyright © Cambridge University Press 1953

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

Daly, R. A., 1935. Igneous Rocks and the Depth of the Earth. New York.Google Scholar
Deer, W. A., 1938. The Diorites and Associated Rocks of the Glen Tilt Complex, Perthshire. I. The Granites and Intermediate Hybrid Rocks. Geol. Mag., lxxv, 174–184.CrossRefGoogle Scholar
Deer, W. A., 1938. The Composition and Paragenesis of the Hornblendes of the Glen Tilt Complex, Perthshire. Miner. Mag., xxv, 56–74.Google Scholar
Deer, W. A., 1950. The Diorites and Associated Rocks of the Glen Tilt Complex, Perthshire. II. Diorites and Appinites. Geol. Mag., lxxxvii, 181–195.CrossRefGoogle Scholar
Nockolds, S. R., 1941. The Garabal Hill—Glen Fyne Igneous Complex. Quart. Journ. Geol. Soc., xcvi, 451–510.Google Scholar
Wiseman, J. D. H., 1934. The Central and South-West Highland Epidiorites: A Study in Progressive Metamorphism. Quart. Journ. Geol. Soc., xc, 354–417.CrossRefGoogle Scholar
Wyllie, B. K. N. and Scott, A., 1913. The Plutonic Rocks of Garabal Hill. Geol. Mag., 1, 503.Google Scholar