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BY:
THOMAS CHINNAPPAN . A ,
M.SC.APPLIED GEOLOGY,
PERIYAR UNIVERSITY,
SALEM.
Clay
Kaolinite
 Crystal system- triclinic .
 Cleavage - perfect basal.
 H-2.
 Sp. gr. - 2.6.
 Lustre - dull earthy.
 Colour-white, sometimes brown or gray.
 Streak - white.
 Habit - clay like masses.
Origin
 Clay minerals most commonly form by
prolonged chemical weathering of silicate
bearing rocks.
 They can also form locally from
hydrothermal activity....
Mode of occurrence
This clay minerals are formed in
Weathering areas.
The clay minerals are formed in in-situ
condition that deposit is called
“Residual deposits”.
Distribution of India
The resources are spread over in a
number of states of which Kerala holds
about 25%.
followed by West Bengal and Rajasthan
(16% each) and Odisha and Karnataka
(10% each).
Uses
They are used in many industrial
application such as paper, paint,
petroleum, ceramic, cement etc…
Kyanite
Kyanite
 Crystal System - triclinic.
 Cleavage - perfect.
 Hard ness – 4.5-7
 Sp. gr. -3.55 -3.66.
 Lustre - vitreous to pearly.
 Colour - usually blue to white, also gray or
green.
 Habit - crystals usually flat.
Origin
The origin of kyanite is metamorphic
origin.
They are formed from high pressure
and temperature.
They mostly occur in medium grade
regional metamorphism
Mode of occurrence
Kyanite occurs in metamorphic
aluminium-rich rocks .
It occurs in gneisses and schists .
Distribution of India
 India has the largest deposits of kyanite in
the world. All the three grades of kyanite are
found here.
 Kyanite grades depend on aluminium
content. Greater the aluminium content,
greater the quality.
 Jharkhand, Maharashtra and Karnataka
produce practically the whole of kyanite of
India.
Jharkhand
 Jharkhand is the largest producer of
kyanite .
 Ores with high degree of purity with
percentages of aluminium silicate
reaching 95 to 97 are found in the
Singhbhum district.
Maharashtra
Maharashtra [second highest producer
of kyanite] produced 14.5 per cent of
the total kyanite in 2002-03.
 Most of the reserves are in Bhandara
district.
Karnataka
 Karnataka is the third largest producer
[5.6 per cent in 2002-03].
 Commercially, workable deposits occur
in Hassan district.
Uses
It is primarily used in metallurgical,
ceramic, refractory, glass, cement
industries due to its ability to stand
high temperatures.
It is also used in making sparking plugs
in automobiles.
Sillimanite
Sillimanite
 Crystal System-orthorhombic.
 Cleavage - perfect .
 H- 6-7.
 Sp. gr.-3.23.
 Lustre- vitreous.
 Colour - brown, pale green or white.
 Habit - long slender crystals, often in parallel
groups.
Origin
 The origin of sillimanite is metamorphic
origin.
 They are formed from high pressure and
high temperature.
 They mostly occur in high-grade regional
metamorphism
Occurrence and uses
The occurrence and uses
of sillimanite are almost
the same as those of
kyanite.
Distribution of India
The main concentration of
Sillimanite is found in Tamil Nadu,
Orissa, Kerala, Andhra Pradesh and
West Bengal.
Orissa is the largest producer of
sillimanite in India. Ganjam district is
an important sillimanite producing
district.
Kerala is the second largest producing
state. The beach sands of Kerala
contain 5 to 6 per cent of sillimanite.
THANK YOU

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Clay,kyanite,sillimanite in economic geology

  • 1. BY: THOMAS CHINNAPPAN . A , M.SC.APPLIED GEOLOGY, PERIYAR UNIVERSITY, SALEM.
  • 3. Kaolinite  Crystal system- triclinic .  Cleavage - perfect basal.  H-2.  Sp. gr. - 2.6.  Lustre - dull earthy.  Colour-white, sometimes brown or gray.  Streak - white.  Habit - clay like masses.
  • 4. Origin  Clay minerals most commonly form by prolonged chemical weathering of silicate bearing rocks.  They can also form locally from hydrothermal activity....
  • 5. Mode of occurrence This clay minerals are formed in Weathering areas. The clay minerals are formed in in-situ condition that deposit is called “Residual deposits”.
  • 6. Distribution of India The resources are spread over in a number of states of which Kerala holds about 25%. followed by West Bengal and Rajasthan (16% each) and Odisha and Karnataka (10% each).
  • 7. Uses They are used in many industrial application such as paper, paint, petroleum, ceramic, cement etc…
  • 9. Kyanite  Crystal System - triclinic.  Cleavage - perfect.  Hard ness – 4.5-7  Sp. gr. -3.55 -3.66.  Lustre - vitreous to pearly.  Colour - usually blue to white, also gray or green.  Habit - crystals usually flat.
  • 10. Origin The origin of kyanite is metamorphic origin. They are formed from high pressure and temperature. They mostly occur in medium grade regional metamorphism
  • 11. Mode of occurrence Kyanite occurs in metamorphic aluminium-rich rocks . It occurs in gneisses and schists .
  • 12. Distribution of India  India has the largest deposits of kyanite in the world. All the three grades of kyanite are found here.  Kyanite grades depend on aluminium content. Greater the aluminium content, greater the quality.  Jharkhand, Maharashtra and Karnataka produce practically the whole of kyanite of India.
  • 13. Jharkhand  Jharkhand is the largest producer of kyanite .  Ores with high degree of purity with percentages of aluminium silicate reaching 95 to 97 are found in the Singhbhum district.
  • 14. Maharashtra Maharashtra [second highest producer of kyanite] produced 14.5 per cent of the total kyanite in 2002-03.  Most of the reserves are in Bhandara district.
  • 15. Karnataka  Karnataka is the third largest producer [5.6 per cent in 2002-03].  Commercially, workable deposits occur in Hassan district.
  • 16. Uses It is primarily used in metallurgical, ceramic, refractory, glass, cement industries due to its ability to stand high temperatures. It is also used in making sparking plugs in automobiles.
  • 18. Sillimanite  Crystal System-orthorhombic.  Cleavage - perfect .  H- 6-7.  Sp. gr.-3.23.  Lustre- vitreous.  Colour - brown, pale green or white.  Habit - long slender crystals, often in parallel groups.
  • 19. Origin  The origin of sillimanite is metamorphic origin.  They are formed from high pressure and high temperature.  They mostly occur in high-grade regional metamorphism
  • 20. Occurrence and uses The occurrence and uses of sillimanite are almost the same as those of kyanite.
  • 21. Distribution of India The main concentration of Sillimanite is found in Tamil Nadu, Orissa, Kerala, Andhra Pradesh and West Bengal.
  • 22. Orissa is the largest producer of sillimanite in India. Ganjam district is an important sillimanite producing district. Kerala is the second largest producing state. The beach sands of Kerala contain 5 to 6 per cent of sillimanite.