Results 211 to 220 of about 15,166 (249)
Mantle-derived fluid flux controls Olympic Dam-style Fe oxide-Cu-Au mineralisation. [PDF]
Thiel S +4 more
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Fossil pollen resolves origin of the South African Proteaceae as transcontinental not transoceanic. [PDF]
Lamont BB, He T, Cowling RM.
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Dual-layered mantle lithosphere beneath southeastern Canadian Cordillera. [PDF]
Huang S, Gu YJ, Johnston ST.
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Zoning of kimberlite provinces and evolution of kimberlite magmatism
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Experimental Study of a kimberlite at Pressures between 42 and 88 Kilobars [PDF]
Ito, Keisuke +2 more
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Indian kimberlites and the genesis of kimberlites
Chemical Geology, 1984Abstract Late Proterozoic kimberlites occur in both southern and central India. They are similar in petrography and geochemistry to the kimberlites of southern Africa and Yakutia, U.S.S.R. These rocks contain low-CaO forsteritic olivines (Fo92), abundant phlogopites, magnesian ilmenites, aluminous—magnesian chromites, chrome-pyrope garnets surrounded
Eric A.K. Middlemost, Dalim K. Paul
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Transportation Research Record: Journal of the Transportation Research Board, 2007
Kimberlite tailings are waste materials left after the recovery of diamond from diamond source rock. The material has a particle size ranging from 20 mm to 75 microns and can be categorized as a soft aggregate. It contains mainly silica, alumina, iron oxide, and magnesia.
R. K. Swami +2 more
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Kimberlite tailings are waste materials left after the recovery of diamond from diamond source rock. The material has a particle size ranging from 20 mm to 75 microns and can be categorized as a soft aggregate. It contains mainly silica, alumina, iron oxide, and magnesia.
R. K. Swami +2 more
openaire +1 more source

