Changes

Jump to navigation Jump to search
no edit summary
Line 77: Line 77:  
|}
 
|}
   −
[[file:exploring-for-stratigraphic-traps_fig21-38.jpg|thumb|{{figure number|2}}.]]
+
==Plays in different margin types==
   −
==Plays in different margin types==
+
[[file:exploring-for-stratigraphic-traps_fig21-38.jpg|left|thumb|{{figure number|2}}Play types for shelf-edge and ramp margins.]]
Different margin types in basins have different play types determined by the geometry and history of the margin. [[:file:exploring-for-stratigraphic-traps_fig21-38.png|Figure 2]] shows play types for shelf-edge and ramp margins.
     −
[[file:exploring-for-stratigraphic-traps_fig21-39.png|left|thumb|{{figure number|3}}See text for explanation.]]
+
Different margin types in basins have different play types determined by the geometry and history of the margin. [[:file:exploring-for-stratigraphic-traps_fig21-38.jpg|Figure 2]] shows play types for shelf-edge and ramp margins.
    
==Example: integrating petrophysics and geology==
 
==Example: integrating petrophysics and geology==
 +
 +
[[file:exploring-for-stratigraphic-traps_fig21-39.png|thumb|{{figure number|3}}Cross section representing the reservoir properties from representative [[capillary pressure]] data.]]
 +
 
Unpublished data (courtesy Amoco Production Company) derived from cores and [[seismic data]] were used to build an integrated lithofacies map. [[:file:exploring-for-stratigraphic-traps_fig21-39.png|Figure 3]] is a cross section representing the reservoir properties from representative [[capillary pressure]] data. The facies belts shown in the map above the cross section were deposited during maximum highstand of the Ismay (Pennsylvanian) carbonates. The fades are superimposed on an isopach map of the highstand systems tract. Test and show data overlain on the map show that significant reservoirs are restricted generally in the ''Ivanovia'' algal mound buildups, which flank a highstand basin shown in gray.
 
Unpublished data (courtesy Amoco Production Company) derived from cores and [[seismic data]] were used to build an integrated lithofacies map. [[:file:exploring-for-stratigraphic-traps_fig21-39.png|Figure 3]] is a cross section representing the reservoir properties from representative [[capillary pressure]] data. The facies belts shown in the map above the cross section were deposited during maximum highstand of the Ismay (Pennsylvanian) carbonates. The fades are superimposed on an isopach map of the highstand systems tract. Test and show data overlain on the map show that significant reservoirs are restricted generally in the ''Ivanovia'' algal mound buildups, which flank a highstand basin shown in gray.
  

Navigation menu