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DIAMOND
Sanjana Dhal
22GEOL028
M.Sc. 1st year
CONTENT
• Introduction
• Properties
• Origin
• Varieties
• Mode of occurrence
• Distribution
• Uses
• Conclusion
Introduction
• Diamond is a rare natural occurring mineral composed of entirely of
carbon.
• This is the only gemstone made up of single element.
• The first diamond was found in India about 800 B.C.
• Diamond’s atom are packed closer together than the atoms of any
other substance.
• Diamond has the highest melting point of any substance(3820 degree
kelvin).
• Diamond conducts heat better than any other substance .
• Diamond having the covalent bond.
GIANTCOVALENTBONDIN DIAMOND
Properties:
• Physical Properties:
• Crystal system-Cubic
• The crystals are mostly octahedral or dodecahedral
• Colour-white,blue,black,reddish,colourless
• Lusture- Admantine
• Cleavage-octahedral
• Fracture-conchoidal
• Specific gravity-3.5
• Hardness -10
• Diagnostic Property-4C (cut,Carat,Clarity&Colour).
Optical Beauty:
• Ability to reflect and refract light.
• Four factors
• Lusture-Quantity and quality of reflecting light.
• Brilliance-Amount of light returned to the eye from the diamond.
• Dispersion-Amount of rainbow colours returned to the eye from the
diamond.
• Scintillation-The sparkle when there is movement by a light source.
Origin:
• Most of the diamond found in the earth surface formed by magmatic
process.
• Some diamond are found in earth by placer deposit.
• Magmatic Process:
• For a ore deposit a source and Host rock are important
• In Diamond, source is lower mantle and host rock is kimberlite &
lamprophyre.
• Kimberlite-A potassic ultrabasic hybrid igneous rock.
• Lamprophyre- A ultrapotassic ultramafic hybrid igneous rock.
• The magma produced due to the partial melting of lower mantle
having low density than the surroundings so it will move towards the
earth surface.
• The magma coming from the lower mantle is enriched in CO2,H2O &
considered as high oxygen fugacity in comparison to upper mantle.
• While reaching the magma in the upper mantle ,due to reducing
environment of upper mantle the CO2 become pure (C) that is in the
form of diamond.
• After the formation of diamond the kimberlite brings the diamond
into the earth surface at a rising speed of 150km/hr.
• Kimberlite brings the diamond from a greater depth & lamprophyre
brings the diamond to the earth surface from shallow depth.
Varieties
• Diamond (proper)-Perfect crystal,transparent .
• Bort-Imperfectly crystallized diamond .
• Ballas-Spheroid aggregates with a radiated structure.
• Carbonado-Black diamond.
Mode of occurence
• Diamond primarily occurs in kimberlite pipe in disseminated manner.
• Age of diamond is older than the host rock i:e kimberlite &
lamprophyre.
• Diamond placer occur more frequently as eluvial placer & alluvial
placers.Ex.-panna
• Diamond also occurs in stratified conglomerate. Ex- Vindhyan
formation & in Kurnool formation.
• Diamond occur as pebbles in sandstone. Ex-panna(Madhya Pradesh).
Distribution
• North- Bundelkhand craton(lamprophyres reported)
• South- Dharwar craton (kimberlite reported)
• Eastern- Gondwana rocks
• Madhya Pradesh:
• Panna(Vindhyan ) shale
• Majhgawan pipe
• Jhiri shale(basal conglomerate )
• Andhra Pradesh:
• Cuddaph
• Anantapur-Wajrakarur diamond mine.
• Kurnool-Bangapalli group(conglomerate & sandstone)
• Krishna & Godavari.
Uses:
• Diamond is the most
valued Gemstone
• Diamond is used in
jewellry making.
• Used in industrial and
technical applications .
• Diamond bits are used
in drilling holes.
Kohinoor:
• The Kohinoor was mined from the Golconda region of Andhra
Pradesh .
• It is one of the largest cut diamond in the world ,original weight is 793
carat & its weight subsequently reduced over centuries & now its
about 105.6 carat(21.12g).
• The Kohinoor diamond was taken away by British east India company
& adorned the crown of Queen Victoria when she becomes the
Empress of India in the year 1877.
• Current owner of Kohinoor is Queen Elizabeth & a part of British
Monarch.
• It is the most expensive diamond in the world.
• Due to its uniqueness , the diamond is said to be Priceless.
Conclusion:
• Diamonds are one of the most unique minerals to be present on
earth.
• With their incredible hardness and unparalleled shine, diamonds have
made their way to not only the top of industries but top of consumer
markets.
Reference:
-A Text Book Of Geology By G.B. MAHAPATRA,CBS Publication.
-Economic Geology By Umeshwar Prasad,CBS Publication.
-Introduction to Ore Forming Processes By Laurence Robb.
Diamond.pptx

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Diamond.pptx

  • 2. CONTENT • Introduction • Properties • Origin • Varieties • Mode of occurrence • Distribution • Uses • Conclusion
  • 3. Introduction • Diamond is a rare natural occurring mineral composed of entirely of carbon. • This is the only gemstone made up of single element. • The first diamond was found in India about 800 B.C. • Diamond’s atom are packed closer together than the atoms of any other substance. • Diamond has the highest melting point of any substance(3820 degree kelvin). • Diamond conducts heat better than any other substance . • Diamond having the covalent bond.
  • 5. Properties: • Physical Properties: • Crystal system-Cubic • The crystals are mostly octahedral or dodecahedral • Colour-white,blue,black,reddish,colourless • Lusture- Admantine • Cleavage-octahedral • Fracture-conchoidal • Specific gravity-3.5 • Hardness -10 • Diagnostic Property-4C (cut,Carat,Clarity&Colour).
  • 6. Optical Beauty: • Ability to reflect and refract light. • Four factors • Lusture-Quantity and quality of reflecting light. • Brilliance-Amount of light returned to the eye from the diamond. • Dispersion-Amount of rainbow colours returned to the eye from the diamond. • Scintillation-The sparkle when there is movement by a light source.
  • 7. Origin: • Most of the diamond found in the earth surface formed by magmatic process. • Some diamond are found in earth by placer deposit. • Magmatic Process: • For a ore deposit a source and Host rock are important • In Diamond, source is lower mantle and host rock is kimberlite & lamprophyre. • Kimberlite-A potassic ultrabasic hybrid igneous rock. • Lamprophyre- A ultrapotassic ultramafic hybrid igneous rock.
  • 8.
  • 9. • The magma produced due to the partial melting of lower mantle having low density than the surroundings so it will move towards the earth surface. • The magma coming from the lower mantle is enriched in CO2,H2O & considered as high oxygen fugacity in comparison to upper mantle. • While reaching the magma in the upper mantle ,due to reducing environment of upper mantle the CO2 become pure (C) that is in the form of diamond. • After the formation of diamond the kimberlite brings the diamond into the earth surface at a rising speed of 150km/hr. • Kimberlite brings the diamond from a greater depth & lamprophyre brings the diamond to the earth surface from shallow depth.
  • 10. Varieties • Diamond (proper)-Perfect crystal,transparent . • Bort-Imperfectly crystallized diamond . • Ballas-Spheroid aggregates with a radiated structure. • Carbonado-Black diamond.
  • 11.
  • 12. Mode of occurence • Diamond primarily occurs in kimberlite pipe in disseminated manner. • Age of diamond is older than the host rock i:e kimberlite & lamprophyre. • Diamond placer occur more frequently as eluvial placer & alluvial placers.Ex.-panna • Diamond also occurs in stratified conglomerate. Ex- Vindhyan formation & in Kurnool formation. • Diamond occur as pebbles in sandstone. Ex-panna(Madhya Pradesh).
  • 13. Distribution • North- Bundelkhand craton(lamprophyres reported) • South- Dharwar craton (kimberlite reported) • Eastern- Gondwana rocks • Madhya Pradesh: • Panna(Vindhyan ) shale • Majhgawan pipe • Jhiri shale(basal conglomerate ) • Andhra Pradesh: • Cuddaph • Anantapur-Wajrakarur diamond mine. • Kurnool-Bangapalli group(conglomerate & sandstone) • Krishna & Godavari.
  • 14.
  • 15. Uses: • Diamond is the most valued Gemstone • Diamond is used in jewellry making. • Used in industrial and technical applications . • Diamond bits are used in drilling holes.
  • 16. Kohinoor: • The Kohinoor was mined from the Golconda region of Andhra Pradesh . • It is one of the largest cut diamond in the world ,original weight is 793 carat & its weight subsequently reduced over centuries & now its about 105.6 carat(21.12g). • The Kohinoor diamond was taken away by British east India company & adorned the crown of Queen Victoria when she becomes the Empress of India in the year 1877. • Current owner of Kohinoor is Queen Elizabeth & a part of British Monarch. • It is the most expensive diamond in the world. • Due to its uniqueness , the diamond is said to be Priceless.
  • 17.
  • 18.
  • 19. Conclusion: • Diamonds are one of the most unique minerals to be present on earth. • With their incredible hardness and unparalleled shine, diamonds have made their way to not only the top of industries but top of consumer markets.
  • 20. Reference: -A Text Book Of Geology By G.B. MAHAPATRA,CBS Publication. -Economic Geology By Umeshwar Prasad,CBS Publication. -Introduction to Ore Forming Processes By Laurence Robb.