Changes

Jump to navigation Jump to search
Line 61: Line 61:  
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.
   −
[[File:CUADROS.png|framed|center|Figure 11A,11B,11C: the deformation sequence of igneous bodies in the host rock]]
+
[[File:CUADROS.png|framed|center|{{figure number|11}}The deformation sequence of igneous bodies in the host rock]]
    
== Acknowledgements ==
 
== Acknowledgements ==

Navigation menu