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- W2041200056 abstract "Abstract The zirconium content is inversely proportional to the hafnium/zirconium ratio in metamorphic rocks surrounding metasomatic granitoid bodies. The zirconium content reaches a maximum in a narrow border just outside the boundaries of the granitoid rocks. Experiments are described to show that such behaviour cannot result from movement of solutions, but could be the result of diffusional transport of material toward the granitoid rocks in a fluid medium." @default.
- W2041200056 created "2016-06-24" @default.
- W2041200056 creator A5070244720 @default.
- W2041200056 date "1968-06-01" @default.
- W2041200056 modified "2023-09-27" @default.
- W2041200056 title "Variations in the hafnium/zirconium ratio of high grade metamorphic rocks from Southeastern Ontario, Canada" @default.
- W2041200056 cites W1975078875 @default.
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- W2041200056 doi "https://doi.org/10.1016/0012-821x(68)90091-5" @default.
- W2041200056 hasPublicationYear "1968" @default.
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