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Intensive Variables in Kimberlite Magmas, Lac de Gras, Canada and Implications for Diamond Survival 总被引：4，自引：4，他引：4
Crystallization temperatures (T) and oxygen fugacities (fO2)of kimberlite magma are estimated from oxides included in olivinephenocrysts from the Leslie, Aaron, Grizzly and Torrie kimberlitepipes in the central Slave Province, Canada. Crystallizationtemperatures recorded by olivine–chromite pairs at anassumed pressure of 1·0 GPa are 1030–1170°C± 50°C, with a mean of 相似文献
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