Page 256 - Petroleum Geology
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CHAPTER  11



            ORIGIN, MIGRATION AND ACCUMULATION OF PETROLEUM:
            DISCUSSION




            SUMMARY

              (1) High-wax crude oil that is found in sediments of  inner neritic, paralic
            or continental facies was probably generated in source rocks stratigraphically
            close to the reservoir.
              (2)  Fields  in  which  the  composition  of  the  crude  oils  and  water  varies
            from reservoir to reservoir probably received their oil from source rocks strati-
            graphically adjacent to the reservoir.
              (3) Fields  and  provinces  in which  petroleum  occurrences and petroleum
            quality are associated  with the sand/shale ratio probably derived their petro-
            leum from source rocks interbedded with the reservoirs.
              (4) Biodegradation of crude oil is evidence of early generation, dominantly
            in rocks of continental and paralic environments, rather than marine. The as-
            sociation of  heavier  crude  oils  with  fresher  formation waters suggests that
            such crudes either have an inherently different composition or tend to be im-
            mature.
              (5) Density  of  crude  oils  is  determined  largely  by  facies  of  the  source
            rock, rather than by temperature and time.
              (6) If  crude oil generated early is heavier than the later, secondary migra-
            tion directions may be dominated by water motion because the critical slope
            may be 10 or 15 times the slope of the potentiometric surface.
              (7) Fields with similar crude oils in reservoirs of different facies probably
            had a source stratigraphically removed from the reservoirs.
              (8) Faults generally act as barriers to lateral migration, but can leak if  the
            vertical  dimension  of  the pooled crude oil or gas is sufficient to generate a
            sufficiently large pressure differential across the fault to another permeable
            rock unit.
              (9) Fields  with  fault  traps  and petroleum  in the same rock unit  in  both
            blocks were either sourced from local source rocks or migration  took place
            during fault movement.
              (10) Faults do not generally act as conduits for petroleum migration.



            EVIDENCE OF STRATIGRAPHIC POSITION OF SOURCE FOR ACCUMULATIONS

              It is a matter of  considerable importance to petroleum geology and the in-
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