Changes

''' Thermal Maturity:''' the intrusion of magma of high temperatures (up to 1200 ° C) has a thermal effect on the country rock can get to promote [[maturation]] of hydrocarbons when diagenetic conditions are not optimal ([[:File:IMAGEN 11.png|Figure 10]]) .

''' Thermal Maturity:''' the intrusion of magma of high temperatures (up to 1200 ° C) has a thermal effect on the country rock can get to promote [[maturation]] of hydrocarbons when diagenetic conditions are not optimal ([[:File:IMAGEN 11.png|Figure 10]]) .

[[File:IMAGEN 11.png|200|thumbnail|center|Figure 10: modeling of the distribution and direction of migration of oil and gas after the intrusion and cooling of a lacolito in the north of the Neuquen Basin and into the Vaca Muerta Formation, in the province of Neuquen, Argentina.]]

[[File:IMAGEN 11.png|400px|thumbnail|center|{{figure number|10}}Modeling of the distribution and direction of migration of oil and gas after the intrusion and cooling of a lacolito in the north of the Neuquen Basin and into the Vaca Muerta Formation, in the province of Neuquen, Argentina.]]

== Conclusions ==

== Conclusions ==

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 ==

== Bibliography ==

== Bibliography ==

 

* Baudino R., D. Delpino, F. Rodriguez Monreal, H. J. Villar, and S. Zencich, 2009, Modeling an atypical petroleum system: A case study of hydrocarbon generation, migration and accumulation related to igneous intrusions in the Neuquen Basin, Argentina: Marine and Petroleum Geology, v. 26, p. 590–605.

* Baudino R., D. Delpino, F. Rodriguez Monreal, H. J. Villar, & S. Zencich, 2009, Modeling an atypical petroleum system: A case study of hydrocarbon generation, migration and accumulation related to igneous intrusions in the Neuquen Basin, Argentina. Marine and Petroleum Geology 26, pp. 590-605.

* Bodet, L., P. Cobbold, O. Galland, J.-B. Gressier, J.-Y. Matthieu, and R. Mourgues, 2010, Control of pore fluid pressure on depth of emplacement of magmatic sills: An experimental approach: Tectonophysics, v. 489, p. 1–13.

* Bodet, L., P. Cobbold, O. Galland, J.-B. Gressier, J.-Y. Matthieu, & R. Mourgues,2010, Control of pore fluid pressure on depth of emplacement of magmatic sills: An experimental approach. Tectonophysics 489, pp. 1-13.

* Gudmundsson, A., and I. F. Lotveit, 2012, Sills as fractured hydrocarbon reservoirs: examples and models: Geological Society (London) Special Publication 374, available online only.

* Gudmundsson, A., & I. F. Lotveit, 2012, Sills as fractured hydrocarbon reservoirs: examples and models. Geological Society, London, Special Publications Online. doi: 10.1144/SP374.5.

* LLambias, E., 2014, Geologia de los cuerpos ígneos: Instituto Superiore de Correlacion Geologica Insugea 15, 220 p.

* LLambias, E., 2014, Geologia de los cuerpos ígneos (2014).

* Menand, T., 2008, The mechanics and dynamics of sills in layered elastic rocks and their implications for the growth of laccoliths and other igneous complexes: Earth and Planetary Science Letters, v. 267, p. 93–99.

* Menand, T., 2008, The mechanics and dynamics of sills in layered elastic rocks and their implications for the growth of laccoliths and other igneous complexes. Earth and Planetary Science Letters 267, pp. 93-99.

* Skarmeta, J., 1993, Mecanismos de emplazamiento, deformacion y transicion de diques a filones manto en sedimentos jurasicos y cretacicos del norte de Chile: Revista geológica de Chile VII, pp. 207–227

* Skarmeta, J., 1993, Mecanismos de emplazamiento, deformacion y transicion de diques a filones manto en sedimentos jurasicos y cretacicos del norte de Chile. Revista geológica de Chile VII, pp. 207-227