Hostname: page-component-78c5997874-s2hrs Total loading time: 0 Render date: 2024-11-04T19:05:51.196Z Has data issue: false hasContentIssue false
  • English
  • Français

The Stratigraphy and Folding of some Metamorphosed Moine Sediments around the Carn Chuinneag and Inchbae granitic gneisses

Published online by Cambridge University Press:  01 May 2009

R. I. Harker
R. I. Harker
Affiliation:
Mineral Sciences Bldg., State College, Pennsylvania, U.S.A.
Get access Rights & Permissions [Opens in a new window]

Abstract

By studying the current bedding in the hornfelsed rocks surrounding the ortho-gneisses of the Carn Chuinneag and Inchbae masses it has been possible to obtain some indication of the stratigraphic order and the nature of the folding of this part of the Moine series.

Type
Articles
Information
Geological Magazine , Volume 93 , Issue 1 , February 1956 , pp. 57 - 62
Copyright
Copyright © Cambridge University Press 1956

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

Harker, R. I., 1954. Further data on the petrology of the pelitic hornfelses of the Carn Chuinneag–Inchbae region, with special reference to the status of almandine. Geol. Mag., xci, 445–462.CrossRefGoogle Scholar
Peach, B. N. et al. , 1912. The geology of Ben Wyvis, Carn Chuinneag, Inchbae, and the surrounding country. Geol. Survey Mem.Google Scholar
Tilley, C. E., 1935. The role of kyanite in the “hornfels-zone” of the Carn Chuinneag granite, Ross-shire. Miner. Mag., xxlv, 92.Google Scholar