Quartz, mica, and amphibole exsolution from majoritic garnet reveals ultra-deep sediment subduction, Appalachian orogen. [PDF]
Keller DS, Ague JJ.
europepmc +1 more source
Attrition in the kimberlite system. [PDF]
Jones TJ, Russell JK.
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Prairie kimberlite study - indicator mineral geochemistry
L H Thorleifson, R G Garrett, G Matile
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Diamondites: evidence for a distinct tectono-thermal diamond-forming event beneath the Kaapvaal craton. [PDF]
Mikhail S +5 more
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Kimberlite indicator minerals and “laterite”, Canadian arctic
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Geochemistry and Glacial Dispersal Patterns of Kimberlite Indicator Minerals in the South Slave Province, NT [PDF]
Dana Campbell +2 more
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Redox reactions in subducted CaCO3-Fe-SiO2 as a potential source of superdeep diamond inclusions. [PDF]
Guo M, Li X, Mao Z, Li F, Li L, Zhou Q.
europepmc +1 more source
Onset of slab mantle melting in Earth's lower mantle: Evidence from ferropericlase in superdeep diamonds. [PDF]
Ni P +15 more
europepmc +1 more source
Decoding kimberlite petrogenesis and advancing diamond exploration: Structural-chemical correlations and deformation analysis of Kimberlite Indicator Minerals [PDF]
Kimberlites have attracted decades of study due to their scientific importance and economic value. However, the complex and hybrid nature of kimberlites has led to ongoing debates and their origin and evolution remain contentious. The rarity of economically viable kimberlites has intensified the need of continued diamond exploration and the development
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