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Seismic fades maps show the areal distribution of seismic fades and are useful when making lithofacies interpretations. The most common and useful parameters to be mapped are seismic reflection patterns and isochrons (thickness measured in seconds of two-way time).

Seismic facies maps show the areal distribution of seismic facies and are useful when making lithofacies interpretations. The most common and useful parameters to be mapped are seismic reflection patterns and isochrons (thickness measured in seconds of two-way time).

==Procedure==

==Procedure==

The table below outlines a suggested procedure for mapping seismic fades.

The table below outlines a suggested procedure for mapping seismic facies.

{| class = "wikitable"

{| class = "wikitable"

[[file:exploring-for-stratigraphic-traps_fig21-28.png|thumb|{{figure number|1}}Modified.]]

[[file:exploring-for-stratigraphic-traps_fig21-28.png|thumb|{{figure number|1}}Modified.]]

[[:file:exploring-for-stratigraphic-traps_fig21-28.png|Figure 1]] contains examples of a seismic fades map, an isochron map, and seismic line A–Á (location shown on maps).

[[:file:exploring-for-stratigraphic-traps_fig21-28.png|Figure 1]] contains examples of a seismic facies map, an isochron map, and seismic line A–Á (location shown on maps).

==See also==

==See also==