Hostname: page-component-cd9895bd7-lnqnp Total loading time: 0 Render date: 2024-12-26T07:56:38.717Z Has data issue: false hasContentIssue false

A naturally occurring sodium vermiculite from Unst, Shetland

Published online by Cambridge University Press:  09 July 2018

C. D. Curtis
Affiliation:
Department of Geology, The University, Sheffield, S1 3JD
P. E. Brown
Affiliation:
Department of Geology, The University, Sheffield, S1 3JD
V. A. Somogyi
Affiliation:
Department of Geology, The University, Sheffield, S1 3JD

Abstract

A naturally occurring macroscopic sodium vermiculite from Unst, Shetland is described. It is similar in many respects to synthetic materials recently prepared from phlogopite by potassium replacement. In other respects, however, it is more akin to macroscopic Mg-vermiculites.

Type
Research Article
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1969

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

Barshad, I. (1950) Am. Miner. 35, 225.Google Scholar
Deer, W.A., Howie, R.A. & Zussman, J. (1962) Rock Forming Minerals Volume 3: Sheet Silicates. Longmans, London.Google Scholar
Newman, A.C.D. (1967) Clay Miner. 7, 215.CrossRefGoogle Scholar
Read, H.H. (1934) Mineralog. Mag. 23, 519.Google Scholar
Shapiro, L. & Brannock, W.W. (1952) Geol. Surv. Amer. Circ. No. 165.Google Scholar
Thompson, T.D., Wentworth, Sally, A. & Brindley, G.W. (1967) Clay Miner. 7, 43.Google Scholar
Walker, G.F. (1961) The X-ray Identification and Crystal Structures of Clay Minerals (Brown, G., editor), Chap. VII, p. 297. Mineralogical Society, London.Google Scholar