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1
New Mexico Diamondiferous Kimberlite
New Mexico Diamondiferous Kimberlite
::2013/05/21::
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2
Kimberlite with precious stone and diamonds natural ore also found
Kimberlite with precious stone and diamonds natural ore also found
::2013/10/19::
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3
Kimberlite with precious stone and diamond natural ore also found
Kimberlite with precious stone and diamond natural ore also found
::2013/10/19::
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4
Kimberlite Zouk vol 1   02   Abysse   La nuit   CLIP
Kimberlite Zouk vol 1 02 Abysse La nuit CLIP
::2013/02/01::
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5
ORE DEPOSITS 101 - Part 2 - Layered Complexes, Kimberlites
ORE DEPOSITS 101 - Part 2 - Layered Complexes, Kimberlites
::2012/06/20::
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6
Diamonds in Yellow and Blue Kimberlite
Diamonds in Yellow and Blue Kimberlite
::2012/12/06::
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7
Kimberlite and diamonds natural
Kimberlite and diamonds natural
::2013/10/28::
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8
Bad boy - kimberlite
Bad boy - kimberlite
::2012/02/08::
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9
Kimberlite Zouk - La Nuit - YourZoukTv - clip officiel
Kimberlite Zouk - La Nuit - YourZoukTv - clip officiel
::2011/09/30::
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10
Kimberlite Zouk - Nehmy - Mon Desir
Kimberlite Zouk - Nehmy - Mon Desir
::2007/04/06::
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11
Kimberlite Zouk Vol 2 (Ls) - C
Kimberlite Zouk Vol 2 (Ls) - C'est Mieux Comme Ca
::2008/12/20::
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12
Kimberlite Zouk Vol I 2004   09   Pit Bacardi & Ruby Mike   Desir Fou
Kimberlite Zouk Vol I 2004 09 Pit Bacardi & Ruby Mike Desir Fou
::2010/08/07::
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13
La Nuit Kimberlite Zouk
La Nuit Kimberlite Zouk
::2012/08/23::
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14
Kimberlite Zouk - La nuit Remix
Kimberlite Zouk - La nuit Remix
::2008/02/12::
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15
Kimberlite with diamonds 6
Kimberlite with diamonds 6
::2013/10/17::
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16
Kimberlite Zouk Vol I 2004   10   Calbo   Chanter La La La
Kimberlite Zouk Vol I 2004 10 Calbo Chanter La La La
::2010/08/07::
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17
UGC-HL Playoffs: Blunderful vs. Kimberlite Council
UGC-HL Playoffs: Blunderful vs. Kimberlite Council
::2013/03/26::
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18
Kimberlite Zouk Vol.I 2004 - 05 - Ommando Toxic and Elpidio - Mes Gars Et Moi
Kimberlite Zouk Vol.I 2004 - 05 - Ommando Toxic and Elpidio - Mes Gars Et Moi
::2010/07/28::
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19
kimberlite pipe and diamonds
kimberlite pipe and diamonds
::2014/05/17::
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20
Terrafirmacraft Ep.7 "KIMBERLITE!?"
Terrafirmacraft Ep.7 "KIMBERLITE!?"
::2014/08/10::
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21
Перевозка буровой на кимберлитовой трубке/ The rig transportation on the kimberlite pipe
Перевозка буровой на кимберлитовой трубке/ The rig transportation on the kimberlite pipe
::2013/10/27::
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22
second hand kimberlite diamond mining plant for sale in south africa grinding mill china
second hand kimberlite diamond mining plant for sale in south africa grinding mill china
::2014/02/08::
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23
KIMBERLITE @ RDF14 Project818 Russian Dance Festival, November 1, Moscow 2014, Top 10 Russia
KIMBERLITE @ RDF14 Project818 Russian Dance Festival, November 1, Moscow 2014, Top 10 Russia
::2014/11/14::
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24
Yakutia. Mirny. Kimberlite pipe (Diamond mining)
Yakutia. Mirny. Kimberlite pipe (Diamond mining)
::2008/08/01::
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25
Kimberlite with other stones
Kimberlite with other stones
::2014/07/03::
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26
KImberlite Zouk Vol 2 Naty mwen laisser vou
KImberlite Zouk Vol 2 Naty mwen laisser vou
::2010/07/29::
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27
KIMBERLITE | RESPECT SHOWCASE RUSSIA
KIMBERLITE | RESPECT SHOWCASE RUSSIA
::2014/11/11::
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28
Kimberlite Diamond Mine
Kimberlite Diamond Mine
::2014/02/13::
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29
Kimberlite in diamonds natural
Kimberlite in diamonds natural
::2014/01/05::
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30
Kimberlite Zouk - Pas de Larmes
Kimberlite Zouk - Pas de Larmes
::2010/02/21::
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31
lakisa nga-Babeth et Ol Kainry dans Kimberlite Zouk
lakisa nga-Babeth et Ol Kainry dans Kimberlite Zouk
::2009/11/13::
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32
Карьер трубки "Айхал" / Aikhal kimberlite pipe open-pit
Карьер трубки "Айхал" / Aikhal kimberlite pipe open-pit
::2013/08/01::
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33
GEN RENARD VIDEO KIMBERLITE R&B 2
GEN RENARD VIDEO KIMBERLITE R&B 2
::2010/02/01::
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34
Kimberlite and diamonds natural
Kimberlite and diamonds natural
::2014/06/04::
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35
Rough diamonds in kimberlite
Rough diamonds in kimberlite
::2014/06/01::
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36
Jordan Rakei - selfish | choreography by Gorbunov Nikita | The First Crew | KIMBERLITE
Jordan Rakei - selfish | choreography by Gorbunov Nikita | The First Crew | KIMBERLITE
::2014/10/12::
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37
15 I don
15 I don't Know - Jalane feat Cedric
::2013/05/23::
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38
kimberlite in Diamonds Natural f
kimberlite in Diamonds Natural f
::2014/07/02::
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39
Kimberlite (Making-Off) Part4
Kimberlite (Making-Off) Part4
::2007/01/21::
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40
Kimberlite in Diamonds Natural 01
Kimberlite in Diamonds Natural 01
::2014/05/17::
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41
kimberlite with rough diamonds and a range of gem stones
kimberlite with rough diamonds and a range of gem stones
::2014/06/10::
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42
Elmasın Oluşumu ve Kimberlite.wmv
Elmasın Oluşumu ve Kimberlite.wmv
::2012/10/12::
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43
Kimberlite in diamond natural
Kimberlite in diamond natural
::2013/10/19::
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44
Magic Plants - Kimberlite [Drumstep]
Magic Plants - Kimberlite [Drumstep]
::2013/05/10::
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45
La ki sa nga Babeth et Ol Kainry dans Kimberlite Zouk
La ki sa nga Babeth et Ol Kainry dans Kimberlite Zouk
::2008/10/22::
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46
Kimberlite and diamonds natural e
Kimberlite and diamonds natural e
::2014/06/04::
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47
Rough Diamonds In Kimberlite
Rough Diamonds In Kimberlite
::2014/06/02::
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48
Kimberlite with precious stone and diamonds natural
Kimberlite with precious stone and diamonds natural
::2014/01/04::
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49
Kimberlite - Let
Kimberlite - Let's See You Top This (Original Unmixed)
::2014/09/30::
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50
Paragon Diamonds looks to progressing its kimberlite project in Lesotho
Paragon Diamonds looks to progressing its kimberlite project in Lesotho
::2012/05/29::
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RESULTS [51 .. 101]
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Kimberlite from U.S.A.
QEMSCAN mineral map of kimberlite from South Africa

Kimberlite is an igneous rock best known for sometimes containing diamonds. It is named after the town of Kimberley in South Africa, where the discovery of an 83.5-carat (16.70 g) diamond in 1871 spawned a diamond rush, eventually creating the Big Hole.

Kimberlite occurs in the Earth's crust in vertical structures known as kimberlite pipes as well as igneous dykes and sills. Kimberlite pipes are the most important source of mined diamonds today. The consensus on kimberlites is that they are formed deep within the mantle. Formation occurs at depths between 150 and 450 kilometres (93 and 280 mi), potentially from anomalously enriched exotic mantle compositions, and are erupted rapidly and violently, often with considerable carbon dioxide and other volatile components. It is this depth of melting and generation which makes kimberlites prone to hosting diamond xenocrysts.

Kimberlite has attracted more attention than its relative volume might suggest that it deserves. This is largely because it serves as a carrier of diamonds and garnet peridotite mantle xenoliths to the Earth's surface. Its probable derivation from depths greater than any other igneous rock type, and the extreme magma composition that it reflects in terms of low silica content and high levels of incompatible trace element enrichment, make an understanding of kimberlite petrogenesis important. In this regard, the study of kimberlite has the potential to provide information about the composition of the deep mantle and about melting processes occurring at or near the interface between the cratonic continental lithosphere and the underlying convecting asthenospheric mantle.

Morphology and volcanology[edit]

Many kimberlites are emplaced as carrot-shaped, vertical intrusions termed 'pipes'. This classic carrot shape is formed due to a complex intrusive process of kimberlitic magma which inherits a large proportion of CO2 (lower amounts of H2O) in the system, which produces a deep explosive boiling stage that causes a significant amount of vertical flaring (Bergman, 1987). Kimberlite classification is based on the recognition of differing rock facies. These differing facies are associated with a particular style of magmatic activity, namely crater, diatreme and hypabyssal rocks (Clement and Skinner 1985, and Clement, 1982).

The morphology of kimberlite pipes, and the classical carrot shape, is the result of explosive diatreme volcanism from very deep mantle-derived sources. These volcanic explosions produce vertical columns of rock that rise from deep magma reservoirs. The morphology of kimberlite pipes is varied but generally includes a sheeted dyke complex of tabular, vertically dipping feeder dykes in the root of the pipe which extends down to the mantle. Within 1.5–2 km (0.93–1.24 mi) of the surface, the highly pressured magma explodes upwards and expands to form a conical to cylindrical diatreme, which erupts to the surface. The surface expression is rarely preserved, but is usually similar to a maar volcano. The diameter of a kimberlite pipe at the surface is typically a few hundred meters to a kilometer (up to 0.6 mile).

Two Jurassic kimberlite dikes exist in Pennsylvania. One, the Gates-Adah Dike, outcrops on the Monongahela River on the border of Fayette and Greene Counties. The other, the Dixonville-Tanoma Dike in central Indiana County, does not outcrop at the surface and was discovered by miners.[1]

Petrology[edit]

Both the location and origin of kimberlitic magmas are areas of contention. Their extreme enrichment and geochemistry has led to a large amount of speculation about their origin, with models placing their source within the sub-continental lithospheric mantle (SCLM) or even as deep as the transition zone. The mechanism of enrichment has also been the topic of interest with models including partial melting, assimilation of subducted sediment or derivation from a primary magma source.

Historically, kimberlites have been subdivided into two distinct varieties termed 'basaltic' and 'micaceous' based primarily on petrographic observations (Wagner, 1914). This was later revised by Smith (1983) who renamed these divisions Group I and Group II based on the isotopic affinities of these rocks using the Nd, Sr and Pb systems. Mitchell (1995) later proposed that these group I and II kimberlites display such distinct differences, that they may not be as closely related as once thought. He showed that Group II kimberlites actually show closer affinities to lamproites than they do to Group I kimberlites. Hence, he reclassified Group II kimberlites as orangeites to prevent confusion.

Group I kimberlites[edit]

Group-I kimberlites are of CO2-rich ultramafic potassic igneous rocks dominated by a primary mineral assemblage of forsteritic olivine, magnesian ilmenite, chromium pyrope, almandine-pyrope, chromium diopside (in some cases subcalcic), phlogopite, enstatite and of Ti-poor chromite. Group I kimberlites exhibit a distinctive inequigranular texture caused by macrocrystic (0.5–10 mm or 0.020–0.394 in) to megacrystic (10–200 mm or 0.39–7.87 in) phenocrysts of olivine, pyrope, chromian diopside, magnesian ilmenite and phlogopite, in a fine to medium grained groundmass.

The groundmass mineralogy, which more closely resembles a true composition of the igneous rock, contains forsteritic olivine, pyrope garnet, Cr-diopside, magnesian ilmenite and spinel.

Olivine Lamproites[edit]

Olivine Lamproites were previously called Group II kimberlite or orangeite in response to their mistakenly being considered to only occurring in South Africa. Their occurrence and petrology, however, are identical globally and should not be erroneously referred to as kimberlite.[2] Olivine lamproites are ultrapotassic, peralkaline rocks rich in volatiles (dominantly H2O). The distinctive characteristic of olivine lamproites is phlogopite macrocrysts and microphenocrysts, together with groundmass micas that vary in composition from phlogopite to "tetraferriphlogopite" (anomalously Al-poor phlogopite requiring Fe to enter the tetrahedral site). Resorbed olivine macrocrysts and euhedral primary crystals of groundmass olivine are common but not essential constituents.

Characteristic primary phases in the groundmass include: zoned pyroxenes (cores of diopside rimmed by Ti-aegirine); spinel-group minerals (magnesian chromite to titaniferous magnetite); Sr- and REE-rich perovskite; Sr-rich apatite; REE-rich phosphates (monazite, daqingshanite); potassian barian hollandite group minerals; Nb-bearing rutile and Mn-bearing ilmenite.

Kimberlitic indicator minerals[edit]

Kimberlites are peculiar igneous rocks because they contain a variety of mineral species with chemical compositions that indicate they formed under high pressure and temperature within the mantle. These minerals such as chromium diopside (a pyroxene), chromium spinels, magnesian ilmenite, and pyrope garnets rich in chromium, are generally absent from most other igneous rocks, making them particularly useful as indicators for kimberlites.

These indicator minerals are generally sought in stream sediments in modern alluvial material. Their presence may indicate the presence of a kimberlite within the erosional watershed which produced the alluvium.

Geochemistry[edit]

The geochemistry of Kimberlites is defined by the following parameters:

  • Ultramafic; MgO >12% and generally >15%
  • Ultrapotassic; Molar K2O/Al2O3 >3
  • Near-primitive Ni (>400 ppm), Cr (>1000 ppm), Co (>150 ppm)
  • REE-enrichment[3]
  • Moderate to high LILE enrichment; ΣLILE = >1,000 ppm
LILE = large ion lithophile elements[4]
  • High H2O and CO2

Economic importance[edit]

Kimberlites are the most important source of primary diamonds. Many kimberlite pipes also produce rich alluvial or eluvial diamond placer deposits. About 6,400 kimberlite pipes have been discovered in the world, of those about 900 have been classified as diamondiferous, and of those just over 30 have been economic enough to diamond mine. [5]

The deposits occurring at Kimberley, South Africa were the first recognized and the source of the name. The Kimberley diamonds were originally found in weathered kimberlite which was colored yellow by limonite, and so was called yellow ground. Deeper workings encountered less altered rock, serpentinized kimberlite, which miners call blue ground.

See also Mir Mine and Udachnaya pipe, both in Sakha Republic, Siberia.

The blue and yellow ground were both prolific producers of diamonds. After the yellow ground had been exhausted, miners in the late 19th century accidentally cut into the blue ground and found gem quality diamonds in quantity. The economic importance of the time is that with flood of diamonds being found, the miners were undercutting each other's price of the diamonds and eventually decreased the diamonds' value down to cost in a short time.[6]

Related rock types[edit]

Notes[edit]

  1. ^ Berg, T.M., Edmunds, W.E., Geyer, A.R. and others, compilers (1980). Geologic Map of Pennsylvania: Pennsylvania Geologic Survey, Map 1, scale 1:250,000.
  2. ^ Francis and Patterson, 2009
  3. ^ Nixon, P.H., 1995. The morphology and nature of primary diamondiferous occurrences. Journal of Geochemical Exoloration, 53: 41-71.
  4. ^ Depletion of gold and LILE in the lower crust: Lewisian Complex, Scotland
  5. ^ "Diamond Investing FAQ", Mining.com, February 18, 2014.
  6. ^ "South Africa: A New History of the Development of the Diamond Fields" (1902): New York Times Archives [PDF file], New York Times.

References[edit]

  • Bergman, S. C.; 1987: Lamproites and other potassium-rich igneous rocks: a review of their occurrences, mineralogy and geochemistry. In: Alkaline Igneous rocks, Fitton, J.G. and Upton, B.G.J (Eds.), Geological Society of London special publication No. 30. pp. 103–19
  • Clement, C. R., 1982: A comparative geological study of some major kimberlite pipes in the Northern Cape and Orange free state. PhD Thesis, University of Cape Town.
  • Clement, C. R., and Skinner, E.M.W. 1985: A textural-genetic classification of kimberlites. Transactions of the Geological Society of South Africa. pp. 403–409.
  • Mitchell, R. H., 1995: Kimberlites, orangeites, and related rocks. Plenum Press, New York.
  • Mitchell, R. H.; Bergman, S. C. (1991). Petrology of Lamproites. New York: Plenum Press. ISBN 0-306-43556-X. 
  • Smith, C. B., 1983: Lead, strontium, and neodymium isotopic evidence for sources of African Cretaceous kimberlite, Nature, 304, pp 51–54.
  • Edwards, C. B., Howkins, J.B., 1966. Kimberlites in Tanganyika with special reference to the Mwadui occurrence. Econ. Geol., 61:537-554.
  • Nixon, P.H., 1995. The morphology and nature of primary diamondiferous occurrences. Journal of Geochemical Exoloration, 53: 41-71
  • Wagner, P. A., 1914: The diamond fields of South Africa; Transvaal Leader, Johannesberg.
  • Woolley, A.R., Bergman, S.C., Edgar, AD, Le Bas, M.J., Mitchell, R.H., Rock, N.M.S. & Scott Smith, B.H., 1996. Classification of lamprophyres, lamproites, kimberlites, and the kalsilitic, melilitic, and leucitic rocks. The Canadian Mineralogist, Vol 34, Part 2. pp. 175–186.

External links[edit]

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