Changes

[[File:IMAGEN 2.png|250px|thumbnail|right|{{figure number|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., and 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 number|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., and 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. The focus of this article is aimed at magmatic bodies of small size (2–4 km in diameter and approximately 500 m thick) of laminar geometries and disposal consistent with available subhorizontal sedimentary rocks (Figure 2).

The focus of the article is aimed at magmatic bodies of small size (2-4 km in diameter and approximately 500 m thick) of laminar geometries and disposal consistent with available subhorizontal sedimentary rocks (Figure 2).

=== Location factors ===

=== Location factors ===