Corona Structures Formed by Near-Isochemical Reaction Between Olivine and Plagioclase in a Metamorphosed Dolerite

R. N. England1
Bureau of Mineral Resources Canberra, Australia
1Published with permission of the Director, Bureau of Mineral Resources, Canberra, A.C.T., Australia.

Mineralogical Magazine; September 1974 v. 39; no. 307; p. 816-818; DOI: 10.1180/minmag.1974.039.307.11
© 1974, The Mineralogical Society
Mineralogical Society (