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Merwinite as an artificial mineral1
Published online by Cambridge University Press: 14 March 2018
Extract
In the investigation of the system CaO–MgO–SiO2 by Ferguson and Merwin the orthositicate 3CaO.MgO.2SiO2 was not observed, and the existence of this compound was first proved in 1921 by Larsen and Foshag who detected it in a contact-altered limestone at Crestmore, California, and gave to it the name merwinite. Since then this compound has been found in contact-altered limestones at Scawt Hill, Antrim, near Neihart in the Little Belt Mts. of Montana, and at Velardeña, Mexico. The history of the recognition of merwinite as an artificial mineral is less easy to trace, but it seems that research workers on refractory bricks were the first to recognize its existence. Thus U.S.A. Patents applied for in the years 1934 and 1935 and British Patents applied for on 11.10.1935 and 19.5.1936 by Non-Metallic Minerals Inc. specify merwinite and periclase as the essential constituents of a refractory brick produced by firing mixtures of dolomite and serpentine, dolomite and sand, or impure magnesite and dolomite at temperatures varying between 2700° and 2900° F.
- Type
- Research Article
- Information
- Mineralogical magazine and journal of the Mineralogical Society , Volume 26 , Issue 177 , June 1942 , pp. 225 - 230
- Copyright
- Copyright © The Mineralogical Society of Great Britain and Ireland 1942
Footnotes
Communicated by permission of the Director, Geological Survey and Museum.
References
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page 230 note 1 Communicated by permission of the Director, Building Research Station.
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