Changes

== Factors Controlling The Emplacement Of Magma ==

== Factors Controlling The Emplacement Of Magma ==

[[File:IMAGEN 2.png|250px|thumbnail|right|Figure 2 : Schematic profile of the Neuquen Basin, province of Neuquen, Argentina , where you can see the site of lamellar bodies of Cenozoic age. Taken from Bermúdez & Delpino<ref name=Bermudez>Bermúdez, A., & D. Delpino, 2015, Concentric and radial joint systems within basic sills and their associated porosity enhancement, Neuquén Basin, Argentina: National Council of Scientific and Technical Investigations, Conciet.</ref>]]

[[File:IMAGEN 2.png|250px|thumbnail|right|Figure 2 : Schematic profile of the Neuquen Basin, province of Neuquen, Argentina , where you can see the site of lamellar bodies of [[Cenozoic]] age. Taken from Bermúdez & Delpino<ref name=Bermudez>Bermúdez, A., & D. Delpino, 2015, Concentric and radial joint systems within basic sills and their associated porosity enhancement, Neuquén Basin, Argentina: National Council of Scientific and Technical Investigations, Conciet.</ref>]]

The magmatic emplacement in the crust is not a freak of nature, it is controlled by a number of physical factors. It will highlight the constraints posed by the location of sedimentary basins subvolcanic due to the importance of these as part of hydrocarbon systems.

The magmatic emplacement in the crust is not a freak of nature, it is controlled by a number of physical factors. It will highlight the constraints posed by the location of sedimentary basins subvolcanic due to the importance of these as part of hydrocarbon systems.

[[File:IMAGEN 5.png|300px|thumbnail|left|Figure 4: Diagram relating the fluid pressure with the decrease in resistance of the country rock with increasing depth . Notice how the anisotropy of the medium magnify the value of T ( tensile stress) in the horizontal direction. Taken from Gressier et al 2010.]] [[File:IMAGEN 6.png|400px|thumbnail|center|Figure 5: experiment by Gressier et al 2010 made into a powder through diatomaceous saturated and unsaturated to simulate fluid through the sediment site. Magma was simulated with silicone caulk which behaves as an ideal Newtonian fluid. The conclusion of this experiment is that in a supersaturated fluid medium and the main effort horizontally oriented sill development is full.]]

[[File:IMAGEN 5.png|300px|thumbnail|left|Figure 4: Diagram relating the fluid pressure with the decrease in resistance of the country rock with increasing depth . Notice how the anisotropy of the medium magnify the value of T ( tensile stress) in the horizontal direction. Taken from Gressier et al 2010.]] [[File:IMAGEN 6.png|400px|thumbnail|center|Figure 5: experiment by Gressier et al 2010 made into a powder through diatomaceous saturated and unsaturated to simulate fluid through the sediment site. Magma was simulated with silicone caulk which behaves as an ideal Newtonian fluid. The conclusion of this experiment is that in a supersaturated fluid medium and the main effort horizontally oriented sill development is full.]]

== Consequences Of Construction Sills ==

== Consequences Of Construction Sills ==