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Stratigraphically complex fields are those that exhibit a high degree of vertical and lateral heterogeneity that is directly controlled by the environment of deposition (Table 1). This heterogeneity occurs at all scales (see “[[Geological heterogeneities]]”). It can result in a highly variable distribution of rock properties within one reservoir and the division of a single stratigraphic interval into multiple reservoirs that act as independent, self-contained compartments.
 
Stratigraphically complex fields are those that exhibit a high degree of vertical and lateral heterogeneity that is directly controlled by the environment of deposition (Table 1). This heterogeneity occurs at all scales (see “[[Geological heterogeneities]]”). It can result in a highly variable distribution of rock properties within one reservoir and the division of a single stratigraphic interval into multiple reservoirs that act as independent, self-contained compartments.
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==Degree of hetrogeneity==
 
{| class = "wikitable"
 
{| class = "wikitable"
 
|-
 
|-
 
|+ {{table number|1}}Tentative, relative deposltional heterogeneity ranking of reservoir facies based primarily on texas petroleum fieldsa
 
|+ {{table number|1}}Tentative, relative deposltional heterogeneity ranking of reservoir facies based primarily on texas petroleum fieldsa
 
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|-
! Heterogeneity
   
! Depositional Environment
 
! Depositional Environment
! Rank
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! Heterogeneity Rank
 
|-
 
|-
 
| ''' Siliciclastic Systems '''
 
| ''' Siliciclastic Systems '''

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