A compilation and characterisation of lithics in kimberlite and common maar-diatremes and tephra ring deposits. [PDF]
Fitzgerald MK, White JDL.
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Nanometric mineral inclusions from a fluid-rich diamond: identification, structure, and implications for deep Earth. [PDF]
Wang Y +18 more
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New geochemical and Sr-Nd-Hf isotopic constraints on the genesis of kimberlites and ultramafic lamprophyres from the Adelaide Fold Belt and Gawler Craton, South Australia. [PDF]
Dalton H +3 more
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Light oxygen isotopes in mantle-derived magmas reflect assimilation of sub-continental lithospheric mantle material. [PDF]
Xu JY +5 more
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Trace element systematics constrain the origin of fluids that form gem-quality diamonds. [PDF]
Rakipov A +8 more
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Evidence for oxygen-conserving diamond formation in redox-buffered subducted oceanic crust sampled as eclogite. [PDF]
Aulbach S, Stachel T.
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Primordial neon and the deep mantle origin of kimberlites. [PDF]
Giuliani A +10 more
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Channelized lithospheric erosion shapes the western North American craton margin. [PDF]
Yang X, Liu L, Cao Z.
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Tungsten-182 evidence for an ancient kimberlite source. [PDF]
Nakanishi N +6 more
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The geology of the Singida kimberlite pipes, Tanganyika
Fifty-four kimberlite pipes and dykes cut Precambrian granite in the Singida region of Tanganyika. The pipes range from 60 to 2500 feet in diameter, and occur in clusters and lines. The lines follow fracture zones.
Mannard, George W.
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