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Displacement pressure estimation from sedimentary facies and well logs (view source)
Revision as of 16:45, 18 March 2014
, 16:45, 18 March 2014→Example: Ardjuna basin, Indonesia
==Example: Ardjuna basin, Indonesia==
==Example: Ardjuna basin, Indonesia==
[[file:evaluating-top-and-fault-seal_fig10-49.png|thumb|{{figure number|1}}Data from Vavra et al.<ref name=ch10r87 />).]]
[[file:evaluating-top-and-fault-seal_fig10-49.png|thumb|{{figure number|1}}Range of seal capacities for the different facies. Data from Vavra et al.<ref name=ch10r87 />).]]
The top seal and capillary properties of rocks from the Ardjuna basin (offshore Java, Indonesia) are related to mappable facies.<ref name=ch10r87 /> The Talang Akar Formation consists of deltaic facies ranging from channel sandstones, delta plain shales, and channel abandonment siltstones to prodelta and delta-front shales as well as shelfal carbonates.
The top seal and capillary properties of rocks from the Ardjuna basin (offshore Java, Indonesia) are related to mappable facies.<ref name=ch10r87 /> The Talang Akar Formation consists of deltaic facies ranging from channel sandstones, delta plain shales, and channel abandonment siltstones to prodelta and delta-front shales as well as shelfal carbonates.