Hostname: page-component-cd9895bd7-8ctnn Total loading time: 0 Render date: 2024-12-23T15:56:27.906Z Has data issue: false hasContentIssue false
  • English
  • Français

Anthophyllite-Cordierite-Granulites of the Lizard

Published online by Cambridge University Press:  01 May 2009

C. E. Tilley
Get access Rights & Permissions [Opens in a new window]

Extract

The region of Trelease Mill and Polkernogo, west of St. Keverne, forms one of the type outcrops of the Old Lizard Head Series north of the main Lizard gabbro. This small rather poorly exposed tract is distinguished not only because it has yielded the only recorded cordierite-bearing rocks among the Lizard schists but more particularly on account of the occurrence of the rarer rock types carrying anthophyllite together with abundant cordierite.

Type
Original Articles
Information
Geological Magazine , Volume 74 , Issue 7 , July 1937 , pp. 300 - 309
Copyright
Copyright © Cambridge University Press 1937

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

[1]. Memoir Geol. Surv. (Enaland and Wales), 1912 (Lizard and Meneage).Google Scholar
[2]. Summ. Prog. Geol. Surv. Gt. Britain, 1930 (for 1929), pt. 2, p. 24.Google Scholar
[3]. Min. Mag., xxiv, 1935, p. 181.Google Scholar
[4]. Norsk Geol. Tidsskr., ix, 1926, pp. 174, 181, 183.Google Scholar
[5]. Bull. Comm. Geol. Finlande, 1914, No. 40, p. 180.Google Scholar