1953, 1953
On the use of ore minerals in the interpretation of the stage of metamorphism within the amphibolite and saussurite facies.
2, 3, 4

In the present paper the author draws attention to the possibility of using ore minerals, especially the ex-solutions observable in sulphides, in the interpretation of the metamorphic facies of the host rock. In the present paper he considers most commou ex-solutions characteristic of the range of temperature corresponding to the amphibolite and to the saussurite facies, and applies microscopic observations in explaining hvo not very common mineral assiocations of the rocks.