Surface 0
1000 -
2 0 0 0 -
E
r
Q.
"o 3 0 0 0 -
n
t,..
4 0 0 0
5 0 0 0
6OO0
~ P o r o s i t y
(%)
=
20
4 0
60
!
!
!
!
I
I
- I
I
I
I
- I
-
European Cretaceous
chalks (Scholle)
- - - - - - - - Floridan Cenozoic
limestones(Halley
and Schmoker )
Fig. 9.16. Carbonate burial curves. Compiled from data in Scholle et aL, 1983, and Halley and Schmoker
(1984).
Relationship between facies, diagenesis and ~ in carbonate reservoirs
Fig. 9.17. Diagram showing that, as carbonate diagenesis increases, environmental interpretation diminishes
in relevance as a tool for predicting porosity.
1000 -
2 0 0 0 -
E
r
Q.
"o 3 0 0 0 -
n
t,..
4 0 0 0
5 0 0 0
6OO0
~ P o r o s i t y
(%)
=
20
4 0
60
!
!
!
!
I
I
- I
I
I
I
- I
-
European Cretaceous
chalks (Scholle)
- - - - - - - - Floridan Cenozoic
limestones(Halley
and Schmoker )
Fig. 9.16. Carbonate burial curves. Compiled from data in Scholle et aL, 1983, and Halley and Schmoker
(1984).
Relationship between facies, diagenesis and ~ in carbonate reservoirs
Fig. 9.17. Diagram showing that, as carbonate diagenesis increases, environmental interpretation diminishes
in relevance as a tool for predicting porosity.