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Hydrocarbon reservoirs associated to layered intrusive bodies (view source)
Revision as of 13:38, 4 April 2019
, 13:38, 4 April 2019→Consequences Of Construction Sills
''' 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 ==