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Coal Deposits
Supervision by: Dr. Ahmed M. ZayedSupervision by: Dr. Ahmed M. Zayed
Edited by : Mostafa Abdel Azim MasoudEdited by : Mostafa Abdel Azim Masoud
Beni-Suef University- EgyptBeni-Suef University- Egypt
Age of Coal Deposits
Majority of the coal deposits are
Pennsylvanian (P) in age; no
coal deposits that are older than
the Devonian (D(.
Land plants had not fully evolved
prior to Devonian therefore coal
deposits which are the remains of
plants could not have formed.
It is also a time in geologic
history when major continental
glaciers occurred in the southern
continents.
Note: carboniferous is divided into
-Mississippians
-Pennsylvanian
Note : A maceral is a component, organic in origin, of coal or oil shale. The term
'maceral' in reference to coal is analogous to the use of the term 'mineral' in reference
to igneous or metamorphic rocks. Examples of macerals are inertinite, vitrinite and
liptinite.
Examples of Macerals
The higher the coal rank the
higher the temperature and
pressure of coal formation.
The higher coal ranks have
a higher percent carbon
and less water.
As moisture and volatiles
are driven off during coal
maturation, carbon is left
behind.
The increased carbon
content increases the heat
content (Btu/lb) of the coal.
Coal Ranks and Energy value
In Sinai
1.1.“G.Maghara ", (Jurassic-
Bathonian), and its backup or
reserve is estimated at 52 million
tons.
2."Ayun Mousa“ subsurface coal
deposits that similar in age to
Maghara coal deposits and
backup is estimated at 40 million
tons.
3.Northeast the "Abu Zenimah",
estimated reserve of 75 million
tons.
4.Umm Bogma coal deposits and sme
surrounding areas as Thora and
Beda of Carboniferous age
Occurrence of Coal in Egypt
Maghara Coal Deposits

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Coal deposits

  • 1. Coal Deposits Supervision by: Dr. Ahmed M. ZayedSupervision by: Dr. Ahmed M. Zayed Edited by : Mostafa Abdel Azim MasoudEdited by : Mostafa Abdel Azim Masoud Beni-Suef University- EgyptBeni-Suef University- Egypt
  • 2.
  • 3.
  • 4.
  • 5.
  • 6.
  • 7.
  • 8. Age of Coal Deposits Majority of the coal deposits are Pennsylvanian (P) in age; no coal deposits that are older than the Devonian (D(. Land plants had not fully evolved prior to Devonian therefore coal deposits which are the remains of plants could not have formed. It is also a time in geologic history when major continental glaciers occurred in the southern continents. Note: carboniferous is divided into -Mississippians -Pennsylvanian
  • 9. Note : A maceral is a component, organic in origin, of coal or oil shale. The term 'maceral' in reference to coal is analogous to the use of the term 'mineral' in reference to igneous or metamorphic rocks. Examples of macerals are inertinite, vitrinite and liptinite.
  • 11.
  • 12. The higher the coal rank the higher the temperature and pressure of coal formation. The higher coal ranks have a higher percent carbon and less water. As moisture and volatiles are driven off during coal maturation, carbon is left behind. The increased carbon content increases the heat content (Btu/lb) of the coal. Coal Ranks and Energy value
  • 13.
  • 14.
  • 15.
  • 16. In Sinai 1.1.“G.Maghara ", (Jurassic- Bathonian), and its backup or reserve is estimated at 52 million tons. 2."Ayun Mousa“ subsurface coal deposits that similar in age to Maghara coal deposits and backup is estimated at 40 million tons. 3.Northeast the "Abu Zenimah", estimated reserve of 75 million tons. 4.Umm Bogma coal deposits and sme surrounding areas as Thora and Beda of Carboniferous age Occurrence of Coal in Egypt