2. “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 .
3.
4. Following stages are involved several stages
:- i) Compaction
ii) Recrystallization
iii) Dissolution
iv) Replacement
v) Authigenesis
vi) Cementation
5.
6.
7.
8.
9.
10.
11. 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 .
Editor's Notes
“Compaction” is a physical process arising from the mass of overlying sediments .
Some grains and minerals deposited in a sediment are unstable and during diagenesis and they may recrystallize
Recrystallised grains may undergo dissolution through the following processes of stream load
The precipitation of new minerals within pore spaces of a sediment is referred to as “authigenesis”
If authigenetic mineral precipitate in sufficient quantity then cementation may result .The ions of cementation are derived from porewater and grain dissolution