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The sill type intrusives are important reservoirs of hydrocarbons in sedimentary basins due to intense secondary patency generated both in the country rock and the same intrusive given by fracturing the formation of stratigraphic traps as fold forced and effects thermal maturity they produce hydrocarbons by high temperature.
 
The sill type intrusives are important reservoirs of hydrocarbons in sedimentary basins due to intense secondary patency generated both in the country rock and the same intrusive given by fracturing the formation of stratigraphic traps as fold forced and effects thermal maturity they produce hydrocarbons by high temperature.
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[[File:CUADROS.png|framed|center|Figure 12A,12B,12C: the deformation sequence of igneous bodies in the host rock]]
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[[File:CUADROS.png|framed|center|Figure 11A,11B,11C: the deformation sequence of igneous bodies in the host rock]]
    
== Acknowledgements ==
 
== Acknowledgements ==

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