Page 280 - Petroleum Geology
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PART 2. PETROLEUM GEOLOGY OF TRANSGRESSIVE SEQUENCES


            CHAPTER 12


            FOSSIL CORAL REEFS





            SUMMARY

              (1) Dominant transgressive sequences tend not to be folded, so this is the
            geological context  of  stratigraphic  traps, of  which fossil reefs are probably
            the purest form.
              (2) Reefs become  large petroleum traps when their vertical dimension has
            been  extended by upward growth with  a rising sea level, relatively. It seems
            necessary  for  them to have grown on a permeable  platform  that acted as a
            carrier bed, because the reef organisms themselves were not the source of the
            petroleum.  Ultimately  they  must  be  exterminated  by  drowning  and/or
            smothering by muddy sediment.
              (3) Diagenesis has a marked influence on reservoir properties. Dolomitized
            reefs tend to be more porous and permeable  than limestone reef  reservoirs,
            and they are also more common.
              (4) Fossil  reefs  commonly  contain  very  large  quantities  of  recoverable
            petroleum and are capable of  producing it at a great rate. Crude oil quality
            tends to be rather heavier than that from sandstone reservoirs, with relatively
            high sulphur content, but no wax.



            INTRODUCTION

              The most remarkable feature of  dominantly transgressive sequences is that
            they tend not to be folded.  The corollary  for petroleum geology is that this
            is  the habitat of  stratigraphic  traps. Fossil coral reefs are arguably the purest
            form of  stratigraphic trap; they are strongly associated with transgressive se-
            quences  that  have  almost  invariably  not  been  folded, whatever  their  age,
            with regional dips commonly less than 5",  many less than 1". When fossil reefs
            become  petroleum  reservoirs,  they  can  contain  very  large quantities of  oil
            and gas, and individual wells are usually very productive.
              We  must  be careful with terminology because the detailed terminology of
            present-day  reefs  is  rarely  applicable to fossil reefs. There are two separate
            influences on comparisons between modern reefs and subsurface reefs. First,
            the dimension of  time may exaggerate or blur the morphology that existed
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