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Journal ArticleDOI

Geochemistry of the Uintjiesberg kimberlite, South Africa: petrogenesis of an off-craton, group I, kimberlite

TLDR
The Uintjiesberg kimberlite diatreme as mentioned in this paper is a group I, calcite kimbersite that has an emplacement age of ∼100 Ma.
About
This article is published in Lithos.The article was published on 2004-06-01. It has received 86 citations till now. The article focuses on the topics: Kimberlite & Xenolith.

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Geochemistry of South African On- and Off-craton, Group I and Group II Kimberlites: Petrogenesis and Source Region Evolution

TL;DR: In this paper, the authors used bulk-rock geochemical compositions of hypabyssal kimberlites, emplaced through the Archaean Kaapvaal craton and Proterozoic Namaqua-Natal belt, to estimate close-to-primary magma compositions of Group I kimbers.
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Dynamical constraints on kimberlite volcanism

TL;DR: In this article, the authors proposed a four-stage model for kimberlite eruptions to explain the main geological relationships of kimbersites, where the early flow exit conditions are overpressured with choked flow conditions; an exit velocity of ∼200m/s is estimated as representative.
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Geochemistry of hypabyssal kimberlites from Lac de Gras, Canada: Comparisons to a global database and applications to the parent magma problem

TL;DR: In this paper, the Lac de Gras parent magma compositions are compared to those calculated from other localities in Canada, Greenland, South Africa and Russia, and the calculated parent magmas define a range, albeit limited, of viable, yet distinct, kimberlite parent Magma compositions.
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Sr, Nd, and Pb isotope evidence for a mantle origin of alkali chlorides and carbonates in the Udachnaya kimberlite, Siberia

TL;DR: In this paper, the authors present new isotopic data that confirm a mantle origin for these kimberlitic chlorides and carbonates, and constrain the emplacement age as ca. 347 Ma.
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Kimberlite-hosted diamond deposits of southern Africa: A review

TL;DR: Kimberlite-hosted diamond deposits are a long-lived and complex series of processes that first involved the growth of diamonds in the mantle, and later their removal and transport to the earth's surface by kimbllite magmas.
References
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Chemical and isotopic systematics of oceanic basalt : implications for mantle composition and processes

S. S. Sun
TL;DR: In this article, trace-element data for mid-ocean ridge basalts and ocean island basalts are used to formulate chemical systematics for oceanic basalts, interpreted in terms of partial-melting conditions, variations in residual mineralogy, involvement of subducted sediment, recycling of oceanic lithosphere and processes within the low velocity zone.
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Chemical differentiation of the Earth: the relationship between mantle, continental crust, and oceanic crust

TL;DR: In this paper, the average chemical compositions of the continental crust and the oceanic crust (represented by MORB), normalized to primitive mantle values and plotted as functions of the apparent bulk partition coefficient of each element, form surprisingly simple, complementary concentration patterns.
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Nature and composition of the continental crust: A lower crustal perspective

TL;DR: In this article, a three-layer crust consisting of upper, middle, and lower crust is divided into type sections associated with different tectonic provinces, in which P wave velocities increase progressively with depth and there is a large variation in average P wave velocity of the lower crust between different type sections.
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