Changes

* '''Folding:''' the movement of material not only produces fracturing but also the folding of the overlying material. These folds are important because they may constitute important reservoirs and traps, even exploited in several basins in the world (Fig 9).

* '''Folding:''' the movement of material not only produces fracturing but also the folding of the overlying material. These folds are important because they may constitute important reservoirs and traps, even exploited in several basins in the world (Fig 9).

[[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) .