L5 - Diamonds Flashcards

1
Q

What are the primary applications of diamonds?

A

Jewelry.

Industrial applications: cutting and grinding.

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2
Q

Where are diamonds typically found?

A
  • Magmatic deposits: Volcanic pipes (kimberlites).
  • Sedimentary deposits: Placers.
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3
Q

How are diamond sizes measured?

A

In carats (1 carat = 200 mg)

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4
Q

What factors determine the viability of a diamond deposit?

A

Grade and value/quality of individual stones

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5
Q

What are typical grades of diamond deposits?

A

0.05 - 2 carats per ton (ct/t).

  • Example: Canada (3.9 ct/t, $95/ct).
  • Example: Lesotho (0.01 ct/t, $1000/ct).
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6
Q

Which countries lead in diamond reserves by value?

A

Botswana.
Russia.
Angola.
Canada.

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7
Q

What is the main producer of synthetic diamonds?

A

china

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8
Q

What are the key lithologies of kimberlite pipes?

A

Kimberlite: Altered, K- and Mg-rich ultramafic rock with olivine, phlogopite, garnet, diamond xenocrysts, and mantle xenoliths.

Lamproite: Similar but saturated in SiO₂.

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9
Q

What are diatremes?

A
  • Pipe-like volcanic structures cutting through country rock.
  • Formed by explosive eruptions due to volatile-rich magma.
  • Often contain craters with volcanic material.
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10
Q

How deep are kimberlite pipes?

A

1-2 km, with eruption craters at the surface.

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11
Q

What conditions are necessary for diamond formation?

A
  • Depth: 200-300 km in the mantle.
  • Pressure: Found beneath old, thick, cold cratons (Archean crust).
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12
Q

How are diamonds related to cratonic heels?

A

Diamonds form in the cold, stable regions at the base of cratons (heels)

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13
Q

What mantle processes contribute to diamond formation?

A
  • Subduction zones and mantle plumes deliver water to depths, driving partial melting.
  • Conditions align with diamond stability fields.
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14
Q

What global trends link kimberlite age and plate tectonics?

A
  • Kimberlite volcanism correlates with plate reconfigurations, such as rifting and subduction.
  • Examples include mountain-building events and mantle plume activities.
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15
Q

What are placer diamond deposits?

A
  • Secondary sedimentary deposits related to river and offshore processes.
  • Concentrated in ancient river networks and coastal environments
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16
Q

How do placer deposits concentrate diamonds?

A
  • High-density diamonds accumulate in depressions, meander belts, and pockets in river basins.
  • Diamonds resist abrasion and are transported by high-velocity currents.
17
Q

What is the role of Stokes’ law in placer deposits?

A

Density differences allow separation and concentration of diamonds in sediment.

18
Q

What are the main methods for diamond exploration?

A
  • Structural context: Understanding fault lines and regional geology.
  • Indicator mineral sampling: Analyzing heavy minerals associated with kimberlite.
  • Geophysics: Airborne magnetics, resistivity contrasts, and density variations.
19
Q

How are pipe models built during exploration?

A
  • Combine geophysical and drilling data to create 3D models.
  • Determine deposit grade and mining potential.
20
Q

What are the main diamond production methods?

A
  • Kimberlite pipes: Open-pit and underground mining.
  • Alluvial and marine deposits: Sediment dredging and cleaning bedrock
21
Q

How are diamonds beneficiated after mining?

A
  • Crushing and concentration using pans and cyclones.
  • Fine material processed on grease tables.
  • Coarser material separated via X-ray sorters and air jets
22
Q

Why are diamonds considered unique?

A
  • Hardest material known (pure carbon).
  • Used as abrasives and gemstones.
23
Q

What evidence supports diamonds forming in the mantle?

A
  • Inclusions of mantle material.
  • Density and structure of diamonds.
24
Q

What volcanic processes bring diamonds to the surface?

A
  • Explosive kimberlite and lamproite eruptions.
  • These eruptions serve as windows into mantle conditions.
25
Q

What is the link between kimberlite volcanism and tectonics?

A

Kimberlite volcanism is tied to plate tectonic events, such as rifting, subduction, and mantle plumes.