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5.  Applied Source Rock Geochemistry   115


            SUMMARY                                           Acknowled gm  ents  W e  thank L. B. Magoon and W. G. Dow
                                                             f o r their invitation to prepare this paper and G. J. Demaison f o r
              Source rock characterization using geochemical  logs   his  s u ggestion  that  it  be written.  The following people
            and  maps  is  an exercise  in sedimentary  basin  analysis   contributed timely reviews that improved the manuscript: L. B.
            with the objective of identifying the pod of active source   Magoon, 5. C. Teerman, D. K.  Baskin, T.  A.  Edison, G.J.
            rock. The pod of active source rock contributes hydrocar­  Demaison, J.T. Smith, and W.G. Dow. Tables  5.1, 5.2, and 5.3
            bons to the petroleum system.                     were improved by input from D. K. Baskin, L. B. Magoon, and
              This  chapter  emphasizes (1) terms  used  to describe   J. Miles. Concepts for Figures 5.2 and 5.3  were provided by T.
            source  rocks;  (2)  sampling,  preparation,  and analysis   A. Edison and 5. C. Teerman, respectively. 5. D. Northam and
            criteria;  (3)  geochemical logs and their use to describe   B.  R.  Barden  coordinated  the production of figures and text.
            source rocks and petroleum  shows in one  dimension;   W e   thank E. L. Couch and N. Schneidermann for their support
            and (4) geochemical maps and their use for interpolating   and  the management of Chevron Overseas Petroleum Inc. f o r
            between  one-dimensional control points  for  a  three­  permission to publish this work.
            dimensional understanding of the petroleum system.
              Proper use of terms  is critical  for  clearly  describing
            petroleum systems. Some examples of source rock terms   References Cited
            include richness,  kerogen  type,  thermal  maturity,
            product generated,  time generated, and provenance or
            depositional environment.  Source rock organic  richness   Alpern, B., 1970, Classification petrographique des constitu­
            can be poor,  fair,  good,  very  good,  or excellent  (Table   ants organiques fossiles des roches sedimentaires: Revue
            5.1). Kerogen can be described as type  I,  II,  III, or IV   Institut Francais du Petrole et Annual Combustion Liquid,
                                                                Paris, v. 25, p. 1233-1266.
            based on elemental analysis (Table 5.2). Organic petrog­  Bandurski, E., 1982, Structural similarities between oil-gener­
            raphy provides information on organic matter type and   ating kerogens and petroleum asphaltenes: Energy
            thermal maturity,  but  is  currently too imprecise  to   Sources, v. 6, p. 47-66.
            describe generative  potential.  Thermal maturity  is   Barker, C., 1979, Organic geochemistry in petroleum explo­
            divided into immature,  mature, and  postmature based   ration: AAPG Continuing Education Course Note Series
                                                      and       10, 159 p.
            on  such parameters  as vitrinite  reflectance, T  max'
            thermal alteration index (Table 5.3). A source rock can be   Baskin, D. K., 1979, A method of preparing phytoclasts for
            described  as potential  (could generate oil), effective   vitrinite reflectance analysis: Journal of Sedimentary
            (generated  or  currently  generating  oil),  or  spent   Petrology, v. 49, p. 633-635.
            (generated oil). A spent source rock can still generate gas.   Baskin, D. K., and K. E. Peters, 1992, Early generation charac­
            An inactive source rock is not generating oil today, but in   teristics of a sulfur-rich Monterey kerogen: AAPG Bulletin,
                                                                v. 76, p. 1-13.
            the past it  was an active source rock.  The term  "marine   Bernard, B. B., 1978, Light hydrocarbons in marine sediments:
            source rock" implies marine deposition, while the terms   Ph.D. dissertation, Texas A&M University, College Station,
            "marine organic matter"  and  "marine  kerogen"  could   TX, p. 53-62.
            imply an origin from marine organisms. A marine source   Bostick, N. H., and B. Alpern, 1977, Principles of sampling,
            rock  might  contain dominantly land  plant organic   preparation, and constituent selection for microphotom­
            matter.                                             etry in measurement of maturation of sedimentary organic
              Geochemical  logs  of  closely  spaced  Rock-Eva!   matter: Journal of Microscopy, v.  109, p. 41-47.
            pyrolysis  and  TOC,  vitrinite reflectance,  lithology,  mud   Cassani, F., and G. Eglinton, 1986, Organic geochemistry of
            log  gas, and  related  data are  indispensable tools in the   Venezuelan extra-heavy oils, 1. Pyrolysis of asphaltenes: a
            sedimentary  basin evaluation process.  Useful geochem­  technique for the correlation and maturity evaluation of
                                                                crude oils: Chemical Geology, v. 56, p. 167-183.
            ical logs  require  adherence to proper  procedures  for   Clementz, D. M., G. J. Demaison, and A. R. Daly, 1979, Well
            sample  selection,  preparation,  analysis,  and  interpreta­  site geochemistry by programmed pyrolysis:  Proceedings
            tion.  These  logs  identify petroleum source  rocks  (as   of the 11th Annual Offshore Technology Conference,
            potential,  effective,  or  spent), the thermal  maturation   Houston, OTC 3410, v.  1, p. 465-470.
            gradient (including immature,  mature,  and postmature   Cook, A. C., and N. R. Sherwood, 1991, Classification of oil
            zones), and in situ and migrated petroleum shows.   shales,  coals and other organic-rich  rocks:  Organic
              Because  of  the  rapid  and inexpensive screening   Geochemistry, v.  17, p. 211-222.
            methods used,  it is  practical to generate  libraries of   Daly, A. R., and J. D. Edman, 1987, Loss of organic carbon
            geochemical logs that progressively reduce the risk asso­  from source rocks during thermal maturation (abs.):
                                                                AAPG Bulletin, v. 71, p. 546.
            ciated with petroleum exploration  as  a  petroleum   Demaison, G. J., 1984, The generative basin concept, in G.J.
            province becomes more thoroughly sampled. Logs from   Demaison and R. J. Murris, eds., Petroleum Geochemistry
            various  locations can be used  to  map  the  pod  of active   and Basin Evaluation:  AAPG Memoir 35, p. 1-14.
            source rock, regional variations in organic facies, and the   Demaison, G. J., A. J. J. Holck, R. W. Jones, and G. T. Moore,
            volume of generated petroleum. This information can be   1983, Predictive source bed stratigraphy; a guide to
            used  as  input  to  refine  mathematical basin models.   regional petroleum occurrence: Proceedings of the 11th
            Finally, the two-step procedure consisting of screening   World Petroleum Congress, London, v. 2, p. 17-29.
            followed  by  detailed  geochemical  analyses  on selected   Demaison, G. J., and B. J. Huizinga, 1991, Genetic classifica­
            samples reduces cost and simplifies interpretation.   tion of petroleum systems: AAPG Bulletin, v. 75, p.
                                                                1626-1643.
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