On scawtite pseudomorphs after spurrite at Scawt Hill, Co. Antrim
Published online by Cambridge University Press: 14 March 2018
Extract
Scawtite was first described at Scawt Hill as a secondary mineral occurring in vesicles and venules in melilite of a melilite-rich hybrid of the endogenous contact-zone. Since then scawtite has been identified in a gehlenite-vesuvianite-ealcite-rock from the contact-zone of a gabbro in the Little Belt Mountains, Montana. The present note records a further occurrence of scawtite at Scawt Hill in a different patagenesis, viz. in association with and replacing spurrite of the exogenous contact-zone.
- Type
- Research Article
- Information
- Mineralogical magazine and journal of the Mineralogical Society , Volume 25 , Issue 160 , March 1938 , pp. 38 - 40
- Copyright
- Copyright © The Mineralogical Society of Great Britain and Ireland 1938
References
page 38 note 1 Tilley, C. E., Min. Mag, 1930, vol. 22, p. 222.CrossRefGoogle Scholar
page 38 note 2 Taylor, J.H., Amer. Min., 1935, vol 20, p. 126. [M.A. 6–125.]Google Scholar
page 38 note 3 Tilley, C.E., and Harwood, H.F., Min. Mag., 1931, vol. 22, p.445.CrossRefGoogle Scholar
- 1
- Cited by