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pro vyhledávání: '"Michelle A.E. Huminicki"'
Publikováno v:
The Canadian Mineralogist. 38:1233-1249
Magmatic sulfides are generally accepted as forming by segregation of an immiscible sulfide liquid from a host silicate melt. Immiscible sulfides have been observed in many types of igneous rocks; however, some types of plutonic and volcanic rocks la
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::96195c184c8df3a6be95b26255d35944
https://doi.org/10.2113/gscanmin.38.5.1233
https://doi.org/10.2113/gscanmin.38.5.1233
