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Many subsurface studies are focused on rocks below a specific surface area where lateral

LaTeX Math Inline
body--uriencoded--\%7B x, \, y \%7D
 variation of Geothermal Temperature Field maybe insignificant comparing to variation along the true vertical direction 
LaTeX Math Inline
body--uriencoded--\%7B z \%7D
.

This allows using Geothermal Temperature Profile 

LaTeX Math Inline
bodyT_G(z)
 instead of Geothermal Temperature Fieldhappens for example at the lateral scales of a typical Petroleum Field where Geothermal Temperature Field usually simplifies to a laterally constant Geothermal Temperature Profile 
LaTeX Math Inline
bodyT_G(x, \, y, \, z)
. 


Fig. 1.1. A sample of Geothermal Temperature Profile.Fig. 1.2. A sample of Geothermal Temperature Profile with zoom around temperature variations above Neutral Temperature Layer 

Fig. 1.3. A sample of Geothermal Temperature Profile at different time moments.

Fig. 1.4. A sample of Geothermal Temperature Profile at different time moments with zoom around temperature variations above Neutral Temperature Layer 

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