Changes

  | isbn    = 0-89181-602-X

  | isbn    = 0-89181-602-X

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Displacement pressure has been inferred from the relationship between capillary properties and sedimentary facies.<ref name=ch10r87>Vavra, C., L., Kaldi, J., G., Sneider, R., M., 1992, Geological applications of [[capillary pressure]]: a review: AAPG Bulletin, vol. 76, no. 6, p. 840–850.</ref><ref name=ch10r68>Shea, W., T., Schwalbach, J., R., Allard, D., M., 1993, Integrated rock-log evaluation of fluvio-lacustrine seals, in Ebanks, J., Kaldi, J., Vavra, C., eds., Seals and Traps: A Multidisciplinary Approach: AAPG Hedberg Research conference, unpublished abstract.</ref> Two examples demonstrate the ability to construct regional facies maps and then assign maximum limits to the amount of hydrocarbon that could be trapped beneath these seals.

Displacement pressure has been inferred from the relationship between capillary properties and sedimentary facies.<ref name=ch10r87>Vavra, C., L., Kaldi, J., G., Sneider, R., M., 1992, [Geological applications of capillary pressure: a review]: AAPG Bulletin, vol. 76, no. 6, p. 840–850.</ref><ref name=ch10r68>Shea, W., T., Schwalbach, J., R., Allard, D., M., 1993, Integrated rock-log evaluation of fluvio-lacustrine seals, in Ebanks, J., Kaldi, J., Vavra, C., eds., Seals and Traps: A Multidisciplinary Approach: AAPG Hedberg Research conference, unpublished abstract.</ref> Two examples demonstrate the ability to construct regional facies maps and then assign maximum limits to the amount of hydrocarbon that could be trapped beneath these seals.

==Example: Ardjuna basin, Indonesia==

==Example: Ardjuna basin, Indonesia==