Hostname: page-component-cd9895bd7-8ctnn Total loading time: 0 Render date: 2024-12-26T21:14:00.285Z Has data issue: false hasContentIssue false
  • English
  • Français

The Dalradian Succession in the Pass of Brander District, Argyll

Published online by Cambridge University Press:  01 May 2009

J. G. C. Anderson
J. G. C. Anderson
Affiliation:
Carnegie Research Scholar, University of Glasgow.
Get access Rights & Permissions [Opens in a new window]

Extract

Between the Cruachan Granite complex and the Glen Strae fault, to the south-east, and the Pass of Brander fault, to the south-west, there is a strip of Dalradian rocks (Fig. 1). These all lie within 1 in. Sheet 45 (Scot.) of the Geological Survey and are described in the Oban and Dalmally Memoir (Hill, 1908, pp. 19–28; Kynaston, 1908, pp. 38–40). Bailey has later distinguished the three great structural divisions into which he has divided the South-West Highlands. These are, in ascending structural succession: the Ballapel Foundation, represented south-east of the granite by Eilde Flags, Glencoe Quartzite, Leven Schists, and Ballachulish Limestone, and south-west of the same by Leven Schists; the Iltay Nappe, represented in both these positions by Islay Quartzite and Easdale Slates; and the Loch Awe Nappe, represented south of the granite by Ardrishaig Phyllites (Bailey, 1922).

Type
Original Articles
Information
Geological Magazine , Volume 72 , Issue 2 , February 1935 , pp. 74 - 80
Copyright
Copyright © Cambridge University Press 1935

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

Allison, A., 1933. “The Dalradian Succession in Islay and Jura,” Quart. Journ. Geol. Soc., lxxxix, 125–144.CrossRefGoogle Scholar
Bailey, E. B., and Macgregor, M., 1912. “The Glen Orchv Anticline,” Quart. Journ. Geol. Soc., lxviii, 164–178.CrossRefGoogle Scholar
Bailey, E. B., 1922. “The Structure of the South-West Highlands of Scotland,” Quart. Journ. Geol. Soc.., lxxviii, 82–127.CrossRefGoogle Scholar
Bailey, E. B., 1930. “New Light on Sedimentation and Tectonics,” Geol. Mag., LXVII, 77–92.CrossRefGoogle Scholar
Hill, J. B., 1908. In “The Geology of the Country near Oban and Dalmally,” Mem. Geol. Surv.Google Scholar
Kynaston, H., 1908. In “The Geology of the Country near Oban and Dalmally,” Mem. Geol. Surv.Google Scholar
Nockolds, S. R., 1934. “The Contaminated Tonalites of Loch Awe, Argyll,” Quart. Journ. Geol. Soc., xc, 302–321.CrossRefGoogle Scholar
1 in. Sheet 45 (Scot.) of the Geological Survey, 1907; colour-printed without revision, 1926.Google Scholar