21
edits
Changes
Jump to navigation
Jump to search
Line 89:
Line 89: − + + + − [[File:IMAGEN 12.png|framed|left|Figure 12: first stage in the construction of a sill. The levels correspond to greenish mudstones ( E in very low resistance GPa) .]] − [[File:IMAGEN 13.png|framed|center|Figure 13: the sill by injection magmatic growing thicker generating a concavo- planar geometry type (lacolith) and buoyancy force to fold layers.]] − [[File:IMAGEN 14.png|framed|right|Figure 14: last stage of intrusion. Important fracturing is generated at the vertices of lacolith by cooling in turn internally fracture (fracture columnar ) generating an internal reservoir and rock fractures box facilitates migration levels permeable sandy .]]
Hydrocarbon reservoirs associated to layered intrusive bodies (view source)
Revision as of 19:51, 26 June 2015
, 19:51, 26 June 2015no edit summary
to intense secondary patency generated both in the country rock and the same intrusive
to intense secondary patency generated both in the country rock and the same intrusive
given by fracturing the formation of stratigraphic traps as fold forced and effects thermal
given by fracturing the formation of stratigraphic traps as fold forced and effects thermal
maturity they produce hydrocarbons by high temperature (Fig 12,13 and 14).
maturity they produce hydrocarbons by high temperature (Fig 12A, 12B, 12C).