Changes

[[File:IMAGEN 10.png|400px|thumbnail|center|Figure 9: 2D seismic conducted northeast of Rockall basin, North Sea Norway. Observe normal faults as a product to accommodate the [[deformation]] of the fold. Taken from Hansen & Cartwright.<ref>Cartwright, J. & D. M. Hansen, 2006, The three-dimensional geometry and growth of forced folds above saucer-shaped igneous sills. Journal of Structural Geology 28, pp. 1520-1535.</ref>]]

[[File:IMAGEN 10.png|400px|thumbnail|center|Figure 9: 2D seismic conducted northeast of Rockall basin, North Sea Norway. Observe normal faults as a product to accommodate the [[deformation]] of the fold. Taken from Hansen & Cartwright.<ref>Cartwright, J. & D. M. Hansen, 2006, The three-dimensional geometry and growth of forced folds above saucer-shaped igneous sills. Journal of Structural Geology 28, pp. 1520-1535.</ref>]]

''' 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 optima (Fig 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 optima (Fig 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 Fm province of Neuquen, Argentina ]]

[[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 Fm province of Neuquen, Argentina ]]