Abstract
AbstractDiopside-skarns, epidote-skarns, and garnet-skarns together with very coarse amphibole-rocks are produced at the contact of limestone and epidiorite by diffusion of trondhjemitic material along the contact. The amphibole-rocks are unusual types, for the formation which material may have been drawn from the epidiorite side the contact.
Publisher
Cambridge University Press (CUP)
Reference2 articles.
1. The composition and occurrence of garnets;Wright;Amer. Min.,1938
2. On the growth of crystals in the contact zone of granite and amphibolite;Cole;Proc. Roy. Irish Acad.,1905
Cited by
2 articles.
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