Represented by Arindam Mukherjee(M.Sc in
Applied Geology)
 “Diagnesis” is a change in sedimentary rock
which may be a chemical , physical or biological
change after when a sediment is deposited in an
environment and it has been continued until
metamorphism takes over . During diagenesis an
indurated rock is produced from an
unconsolidated loose sediments .At higher
elevated temperature (150 °-200° C) or pressure
diagenesis may occur . Early digenetic event
occur at shallow burial and late digenetic event
occur at deep burial .
 Following stages are involved several stages
:- i) Compaction
 ii) Recrystallization
 iii) Dissolution
 iv) Replacement
 v) Authigenesis
 vi) Cementation
 Digenetic process are important for several
reasons
 i) They can considerably modify a sediment .
 ii) They can also effect sediments porosity
and permeability .
 iii) In rare case original structures of
sedimentary rocks may destroyed .

Digenesis

  • 1.
    Represented by ArindamMukherjee(M.Sc in Applied Geology)
  • 2.
     “Diagnesis” isa change in sedimentary rock which may be a chemical , physical or biological change after when a sediment is deposited in an environment and it has been continued until metamorphism takes over . During diagenesis an indurated rock is produced from an unconsolidated loose sediments .At higher elevated temperature (150 °-200° C) or pressure diagenesis may occur . Early digenetic event occur at shallow burial and late digenetic event occur at deep burial .
  • 4.
     Following stagesare involved several stages :- i) Compaction  ii) Recrystallization  iii) Dissolution  iv) Replacement  v) Authigenesis  vi) Cementation
  • 11.
     Digenetic processare important for several reasons  i) They can considerably modify a sediment .  ii) They can also effect sediments porosity and permeability .  iii) In rare case original structures of sedimentary rocks may destroyed .

Editor's Notes

  • #6 “Compaction” is a physical process arising from the mass of overlying sediments .
  • #7 Some grains and minerals deposited in a sediment are unstable and during diagenesis and they may recrystallize
  • #8  Recrystallised grains may undergo dissolution through the following processes of stream load
  • #10 The precipitation of new minerals within pore spaces of a sediment is referred to as “authigenesis”
  • #11 If authigenetic mineral precipitate in sufficient quantity then cementation may result .The ions of cementation are derived from porewater and grain dissolution