Institution: | Missouri University of Science and Technology |
---|---|
Department: | |
Year: | 1912 |
Record ID: | 1485213 |
Full text PDF: | http://hdl.handle.net/10355/27004 |
"The object of this paper is to arrive at a better explanation of the segregation of magmatic solutions on cooling. In which magmas will be discussed from a chemical and metallurgical lien of reasoning, in showing why such minerals as apatite, magnetite, etc., having a comparatively low melting point, crystallize cut before feldspar and quartz, which have a comparatively high fusion point" – p. [1].