Difference between revisions of "Migration pathway map construction"

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==Example: fault controlling migration==
 
==Example: fault controlling migration==
  
[[file:evaluating-top-and-fault-seal_fig10-32.png|thumb|{{figure number|1}}See text for explanation.]]
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[[file:evaluating-top-and-fault-seal_fig10-32.png|thumb|{{figure number|1}}How a fault can control migration pathways across a fault.]]
  
 
[[:file:evaluating-top-and-fault-seal_fig10-32.png|Figure 1]] illustrates how completely a fault can control [[migration pathways]] across a fault. In this fault plane profile of a fault in a Gulf Coast field, SGR was calculated and contoured only on areas of sand/sand juxtaposition. Areas of sand/shale juxtaposition are uncolored. No hydrocarbon migration will occur across these uncolored regions or across the sand/shale juxtapositions with low SGRs (blue-purple). These high SGR areas are essentially holes for fluid migration in the fault plane. It will only occur across the areas of sand/sand juxtaposition with high SGRs (red-orange).
 
[[:file:evaluating-top-and-fault-seal_fig10-32.png|Figure 1]] illustrates how completely a fault can control [[migration pathways]] across a fault. In this fault plane profile of a fault in a Gulf Coast field, SGR was calculated and contoured only on areas of sand/sand juxtaposition. Areas of sand/shale juxtaposition are uncolored. No hydrocarbon migration will occur across these uncolored regions or across the sand/shale juxtapositions with low SGRs (blue-purple). These high SGR areas are essentially holes for fluid migration in the fault plane. It will only occur across the areas of sand/sand juxtaposition with high SGRs (red-orange).

Revision as of 14:43, 1 May 2014

Exploring for Oil and Gas Traps
Series Treatise in Petroleum Geology
Part Predicting the occurrence of oil and gas traps
Chapter Evaluating top and fault seal
Author Grant M. Skerlec
Link Web page
Store AAPG Store

A migration pathway map is a fundamental tool for prospect assessment and field development. In simple migration pathway maps, arrows are drawn perpendicular to structural contours. However, migration pathway maps must also define those faults and those parts of faults that juxtapose sand/sand as well as those faults that cross-seal/cross-leak and dip-seal/dip-leak.

Requirements for map construction

The following table lists the requirements for constructing a migration pathway map.

Requirement Explanation
Structure–depth maps Defines buoyant vectors for hydrocarbon migration
Fault plane profile Defines sand/sand and sand/shale juxtaposition and potential juxtaposed lithology leak points (JLLPs)
Quantitative fault plane analysis Defines real JLLPs, areas of cross-seal or cross-leak, and areas of dip seal or dip leak

Example: fault controlling migration

Figure 1 How a fault can control migration pathways across a fault.

Figure 1 illustrates how completely a fault can control migration pathways across a fault. In this fault plane profile of a fault in a Gulf Coast field, SGR was calculated and contoured only on areas of sand/sand juxtaposition. Areas of sand/shale juxtaposition are uncolored. No hydrocarbon migration will occur across these uncolored regions or across the sand/shale juxtapositions with low SGRs (blue-purple). These high SGR areas are essentially holes for fluid migration in the fault plane. It will only occur across the areas of sand/sand juxtaposition with high SGRs (red-orange).

See also

External links

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Migration pathway map construction
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