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===Stratigraphic cross sections===
 
===Stratigraphic cross sections===
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Lateral variability in facies relationships, and thus reservoir continuity and heterogeneity, are best determined from the construction of stratigraphic [[cross section]]s. An example of a cross section through part of a tight gas reservoir is shown in [[:file:evaluating-tight-gas-reservoirs_fig2.png|Figure 2]]. Facies interpretations are based on [[core description]]s and extrapolation of log signatures for each cored facies to adjacent uncored wells. Distributary channel sandstones form the reservoirs, and bay, marsh, and crevasse splay mudstones form the seal. The lack of production in the two wells to the east is attributed to the pinching out of these mudstone facies and substantiates its importance as a stratigraphic seal. Note the laterally discontinuous nature of individual reservoir sandstone beds as depicted in the cross section.
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[[Lateral]] variability in facies relationships, and thus reservoir continuity and heterogeneity, are best determined from the construction of stratigraphic [[cross section]]s. An example of a cross section through part of a tight gas reservoir is shown in [[:file:evaluating-tight-gas-reservoirs_fig2.png|Figure 2]]. Facies interpretations are based on [[core description]]s and extrapolation of log signatures for each cored facies to adjacent uncored wells. [[Distributary channel]] sandstones form the reservoirs, and bay, marsh, and crevasse splay [[mudstones]] form the seal. The lack of production in the two wells to the east is attributed to the pinching out of these mudstone facies and substantiates its importance as a stratigraphic seal. Note the laterally discontinuous nature of individual reservoir sandstone beds as depicted in the cross section.
    
===Petrophysical properties of reservoir facies===
 
===Petrophysical properties of reservoir facies===
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[[Category:Geological methods]]
 
[[Category:Geological methods]]
 
[[Category:Play type]]
 
[[Category:Play type]]
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[[Category:Methods in Exploration 10]]

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