In this setting the roof sequence frequently develops passive roof duplexes banks and warburton 1986.
Roof thrust duplex.
Two flat segments called thefloor and roof thrusts connected by several parallel ramp segments.
Sole thrust at the base and by a roof thrust at the top mcclay 1992.
Source for information on roof thrust.
Also upper and lower detachments have been described in a similar context for fold duplex structures dahlstrom 1969a.
Else in the world.
Roof thrust in a duplex system the structurally highest bounding thrust surface which joins the floor thrust at the leading and trailing edges of the duplex.
Thrust duplex duplexes occur where there are two decollement levels close to each other within a sedimentary sequence such as the top and base of a relatively strong sandstone layer bounded by two relatively weak mudstone layers.
The fault bound bodies of rock in the duplex are called horses.
Blind thrusts are those below the erosion surface but their presence is indicated by shortening in the overlying sequence which is achieved by disharmonic.
Duplexes have a variety of forms and sizes depending on the amount of displacement of the individual horses.
Boyer and elliott 1982 state that the roof thrust of a duplex is initiated as a major thrust.
A dictionary of earth sciences dictionary.
The rock masses bounded by these faults are calledhorses and the entire structural association is a duplex.
A duplex as a reminder is an array of thrust horses bounded by a floor thrust i e.
Duplex structures are a system of imbricate thrust faults that branch off from a floor thrust below and curve upward to join a roof thrust at a branch line.
The central appalachian fold thrust belt is characterized by a passive roof duplex and as such the total shortening accom modated by the sequence above the roof thrust must equal the shortening.
In a thrust envi ronment the structural association is.
The sicilian collisional complex is a well exposed fold and thrust belt ftb belonging to the apennine maghrebian chain developed along the africa europe plate margin fig.
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