The modern Igwisi Hills kimberlite volcanoes (4° 53′ 19.22″ S, 31° 55′ 59.15″ E) are located at the western margin of the Tanzania craton (Fig. 1), where the magmas erupted through gneisses of the Archaean Dodoman system (Bell and Dodson 1981).The volcanoes comprise three exceptionally well-preserved sub-circular volcanic centres (NE, …
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The central Lac de Gras (LDG) kimberlite field, which contains the Diavik and Ekati Diamond Mines, was principally active from 75 to 45 Ma (Cretaceous to Eocene) (Sarkar et al. 2015). The LDG field is located east of the inferred craton suture (Fig. 1). Its kimberlite pipes define a 100-km by 200-km northwest-trending zone (Lockhart et al. …
The concept encompassed in Table 1 is partly inspired by the approach of McPhie et al. and has some similarities to Cas et al. (2008, 2009).However, there are key differences between our scheme for kimberlite nomenclature and these approaches. Most critically, McPhie et al. and Cas et al. (2008, 2009) begin with an initial textural …
Djerfisherite (K 6 (Fe,Ni,Cu) 25 S 26 Cl) occurs as an accessory phase in the groundmass of many kimberlites, kimberlite-hosted mantle xenoliths, and as a daughter inclusion phase in diamonds and kimberlitic minerals. Djerfisherite typically occurs as replacement of pre-existing Fe–Ni–Cu sulphides (i.e. pyrrhotite, pentlandite and …
Fig. 2 shows the temporal distribution of global kimberlite occurrences (those with available age dates) in the form of a frequency distribution with a bin size of 25 Myr. Kimberlite magmatism occurred episodically since ca. 2.85 Ga (cf., de Wit et al., 2016), and the overall frequency increases significantly toward the …
This alludes to a proto-kimberlite melt which contains higher concentrations of alkali-carbonates, chlorides and phosphates than commonly measured in whole-rock analyses (e.g., Le Roex et al., 2003, Becker and Le Roex, 2006, Nielsen and Sand, 2008, Kjarsgaard et al., 2009). Although unconstrained in their concentration in the proto …
The reaction of orthopyroxene with the kimberlite-related melt has led to orthopyroxene dissolution and formation of the CMI, the latter being surrounded by complex reaction zones and containing zoned olivine grains with extremely high-Mg# (up to 99) cores. This report highlights the utility of minerals present in minor volume proportions in ...
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1) Crater Facies Kimberlite 2) Diatreme Facies Kimberlite 3) Hypabyssal Facies Kimberlite ♦ 1) Crater Facies: The surface morphology of un-weathered kimberlite (Fig.1) is characterized by a crater, up to 2 km in diameter, whose floor may be 150 to 300 m below the surface. The crater is generally deepest in the middle and round the crater is a ...
Some models prefer kimberlite melt origins from mantle plume sources (Le Roex, 1986, Haggerty, 1994, Summary and conclusion Integration of a wide variety of datasets (geochronology, isotope geology, experimental petrology, volcanology, paleogeography; Supplementary files A to E) enables us to refine existing models for the …
Kimberlite chemical composition. Kimberlite is a potassic to ultrapotassic magnesium oxide-rich (15-27 wt. % MgO), silica-poor (20-36 wt.% SiO 2) ultramafic rock. This rare rock is rich in volatiles, incompatible elements, and rare Earth elements (REE) and has considerable iron and calcium oxides.
kimberlite based on microdiamonds Johannes Ferreira To cite this version: Johannes Ferreira. Sampling and estimation of diamond content in kimberlite based on micro-diamonds. Other. Ecole Nationale Supérieure des Mines de Paris, 2013. English. NNT: 2013ENMP0078. pastel-00982337
The presence of the Archean Craton.The study area lies in the southern margin of the Archean Kaapvaal Craton (Fig. 2 a) which is known to host diamondiferous kimberlites (Gurney et al., 1993).Download : Download high-res image (597KB) Download : Download full-size image Fig. 2. (a) Various Archean volcano-sedimentary sequences, …
The Udachnaya diamondiferous kimberlite pipe is located in the northwestern part of the Daldyn–Alakit kimberlite province in Siberia (Fig. 1).At the surface, two adjacent kimberlite bodies (East and West) are recognised, and these can be traced to separate pipes in underground workings beyond ~ 250–270 m.Based on stratigraphic …
The purpose of this study was to examine the viability of using a hand-held portable X-ray fluorescence (pXRF) spectrometer to rapidly obtain geochemical data on kimberlite samples, and thus enable discrimination of different kimberlite phases. Potential applications range from augmenting core logging at the exploration stage, to ore grade …
Overall, the relative kimberlite potential at kimberlite locations is greater for Case 2 than for S40RTS (Fig 9E and 9F): the peak in the number of kimberlites is for a relative kimberlite potential of about 0.3 for S40RTS (median 0.21 and mean 0.19) and about 0.55 for Case 2 (median 0.24 and mean 0.35) over 320 Ma (Fig 9E); over 640 Ma …
These systems are based on the property of diamonds having a much higher specific gravity (density) of ~352 g/cm3 compared to most of the other minerals that make up material in which diamonds are found The first stage of kimberlite processing is to crush and screen the Once a diamond operation yields ore, the diamonds must be sorted from the ...
The Letšeng-la-Terae kimberlite (Lesotho), famous for its large high-value diamonds, has five distinct phases that are mined in a Main and a Satellite pipe. These diatreme phases are heavily altered but parts of a directly adjacent kimberlite blow are exceptionally fresh. The blow groundmass consists of preserved primary olivine with …
This study aims to constrain the nature of kimberlite–xenolith reactions and the fluid origin for Kimberley-type pyroclastic kimberlite (KPK). KPKs are characterized by an abundance of basement xenoliths (15–90%) and display distinct pipe morphology, textures, and mineralogy. To explain the KPK mineralogy deviating from the mineralogy …
Kimberlite originates in the upper portion of the mantle, and it is one of the few stones that do so. Kimberlite "pipes" are actually shaped a bit like a carrot, widening at the top. The pipes are the remnants of ancient, deep volcanos. The source of kimberlite lies almost 300% deeper in the Earth than most volcanoes.
Abstract The paper presents a comprehensive review of currently available data on melt inclusions entrapped in minerals of kimberlites of different age and different provenance in ancient cratons. The crystallized melt inclusions represent snapshots of kimberlite melts at different stages of their evolution. All of the inclusions are completely …
Déjà en 1887, C. Lewis classifia la kimberlite en 3 grandes sortes: 1. La kimberlite massive, porphy¬rique, une masse homogène ayant peu d'inclusions de ro-ches satellites, de couleur gris sombre, lourde et dure. 2. La brèche kimberlitique, plus tendre, conglomérat d'élé¬ments kimberlitiques différents liés par un ciment (matrice).
The material referred to as kimberlite, also called blue ground, is a dark-colored, often fragmented, intrusive rock that may contain diamonds in its rock matrix. It is named after the town of Kimberley, South Africa, where in 1869 the discovery of an 83 carat diamond inside kimberlite rock spawned the world's largest diamond rush.
Kimberlite magma can rise toward the surface at speeds estimated at up to 400 meters (1,200 feet) per second, ripping up more and more pieces from the surrounding rock, which gives the kimberlite its characteristic texture (fig. 3). Figure 2--Generalized diagram of a kimberlite pipe. Figure 3--Polished kimberlite core sample.
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