Emplacement conditions of some Lac de Gras kimberlites and their effect on the resorption of diamonds
Crystallization temperatures (T) and oxygen fugacities (fO2) of kimberlite magma estimated from oxides included in olivine phenocrysts from eight kimberlite pipes in the central Slave Province, Canada, are compared to the degree and character of resorption observed in diamonds recovered from these k...
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Language: | English en |
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2010
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Online Access: | http://hdl.handle.net/1828/2154 |