Attempt on Regional Situation Analysis, Conceptual Resource Estimation and Procedure of Strategic Decision-Making in Planning and Conduct of Exploration and Appraisal Operations (Example of the South Caspian Basin) - Fluid Dynamics of Oil and Gas Reservoirs - page 565

Temperature at minus
1,000 m subcrop

° C t − 1000

<29.5
and
>43.0

<27.0 and
>47.0

<27.0 and
>45.0

<32.0 and
>59.0

<51.0 and
>59.5

<32.0 and
>55.0

<41,0 and
>55,0

Average geothermal
gradient

° C/km G <15.00

and
>18.40

<12.50
and
>18.00

<11.90 and
>16.70

<14.50
and
>18.40

<13.80
and
>23.00

<14.40 and
>16.70

<15,50
and
>19,00

Temperature nor-
malized to base
of Productive
Sequence (Red-
Bed Sequence)

t PS(RS) <18.5

and
>23.3

<18.0 and
>25.0

<16.5 and
>23.0

<19.0 and
>63.0

<26.0 and
>43.0

<19.4 and
>29.7

<24,0 and
>26,5

° C/km

Heat low normal-
ized to base
of Productive
Sequence (Red-
Bed Sequence)

10 − 8 cal/
cm 2

q PS(RS) <11.0

and
>26.0

<12.7 and
>22.8

<9.5 and
>18.5

<17.0 and
>110.0

<24.0 and
>47.0

<10.8 and
>39.6

<26,5 and
>32,2 − s/km

МPa/ МPa P ADP

Formation pres-
sure super-
hydrostaticity
factor

<1.200
and
>1.580

<1.130
and
>1.630

<1.260 and
>1.540

<1.025
and
>1.173

<1.085
and
>1.490

<1.320
and
>1.540

<1,480
and
>1,775

Depth to surface of
AHFP zone

m D ADP <750 and

>2100

<790 and
>1225

<730 and
>1080

<855 and
>935

<875 and
>1350

<640 and
>860

<1300
and
>1600

( Continues )