Page 131 - Origin and Prediction of Abnormal Formation Pressures
P. 131

Geothermal gradient
                       Contents of various clay minerals, pore pressure gradient in shales, and geothermal gradient in the various oil and gas fields of Azerbaijan and the South Caspian
                             Pore pressure gradient
                         Basin (average values are shown in parentheses) (after Buryakovsky et al., 1995, table 4, p. 210)
                                Kaolinite   C'CIkm)   (MPa/m)  Mixed-layer   Chlorite   0.0135   Trace   Trace-5   20   (3.8)   0.0146   Trace-5   Trace   15-20   (2.5)   (17.5)   0.0171   Trace-5   Trace-15   10-35   (1)   (6)   (24)   0.0176   Trace   Trace-10   10-15   (5)   (12.5)   16.0   0.0176   Trace- 15   Trace-20   (10)   (12)
                             Clay mineral content (%)   Hydromica  Montmorillonite   45-60   10-35   (51)   40   10-35   5-60   (24)   10-45   (28)   10-53   40-75   (23)







                                          (24)
                                             40
                                                       Island   (41)   30-75   (49)   (53)








                   TABLE 4-5   Area   Bibieibat   Gryazevaya Sopka   Gyuneshli   Bakhar   Sangachaly-Duvanny-Bulla   Kyurovdag, Karabagly
   126   127   128   129   130   131   132   133   134   135   136