Page 333 - Petroleum Geology
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PART 3. PETROLEUM GEOLOGY OF REGRESSIVE  SEQUENCES


            CHAPTER 14



            ABNORMAL PRESSURES




            SUMMARY

              (1) Abnormal pressures are, for practical purposes, pore pressures that are
            sufficiently greater than normal hydrostatic to have a noticeable effect when
            drilling, and to require special precautions. They are stratigraphically related
            to thick mudstones,  usually but not invariably in regressive sequences, with
            sand/shale ratios less than 10%.
              (2) Abnormally  high pore  pressures are also related to growth  structures
            that are also stratigraphically related - that is, to those that occur in regressive
            sequences. The top of abnormal pressures usually lies below the level of maxi-
            mum  growth-rate  on growth  faults,  close  to (above  or  below) the level at
            which growth faulting began. These relationships appear to be causal.
              (3) The cause of  abnormal pressures is largely mechanical loading of a rela-
            tively impermeable mudstone, and it seems likely that the pore pressures in
            such mudstones have never been normal hydrostatic. In their turn, they cause
            mechanical instability  in such regressive sequences through the retention  of
            relatively large porosity, low bulk density and low equivalent viscosity while
            the sandier part of the regressive sequence accumulates.
              (4) Generation of  petroleum  in the source rock may also generate abnor-
            mal pressures (and resistivities higher than normal).



            OBSERVATIONS

              There  is  a  great  deal  of  evidence  from boreholes around the world that
            pore-fluid pressures are, in general, normal hydrostatic - that is, the pressures
            measured in water reservoirs and the water legs of  oil reservoirs are sufficient
            to support a column of  that water to close to the land surface (or sea level
            on the continental  shelves). This  implies that the pore water is in physical
            continuity  to the surface,  however tortuous the paths may be, and that dur-
            ing  burial  this  continuity  has been maintained. Were  it not for the ever-in-
            creasing depths of  boreholes  drilled for petroleum,  it might reasonably have
            been assumed that this was the universal rule.
              The  drilling  of  “gushers”  in  the  cable-tool days  does  not  constitute  an
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