Progressive metasomatism in the flint nodules of the Scawt Hill contact-zone
Published online by Cambridge University Press: 14 March 2018
Extract
In describing the chief assemblages of the Scawt Hill contact-zone in Co. Antrim brief reference was made to the occurrence of wollastonite and xonotlite associated with the flint nodules of the contact-altered chalk. A more detailed examination of these nodules has now been made and the study of a large number of examples has revealed an interesting group of mineral assemblages which have developed by a progressive metasomatism of these siliceous bodies.
- Type
- Research Article
- Information
- Mineralogical magazine and journal of the Mineralogical Society , Volume 23 , Issue 144 , March 1934 , pp. 513 - 518
- Copyright
- Copyright © The Mineralogical Society of Great Britain and Ireland 1934
References
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