The Occurrence of an Orthorhombic High-Temperature Form of Ca2SiO4 (Bredigite) in the Scawt Hill Contact-Zone and as a Constituent of Slags

C. E. Tilley and H. C. G. Vincent
Department of Mineralogy and Petrology, University of Cambridge.

Mineralogical Magazine; March 1948 v. 28; no. 200; p. 255-271; DOI: 10.1180/minmag.1948.028.200.02
© 1948, The Mineralogical Society
Mineralogical Society (www.minersoc.org)