Source for information on roof thrust.
Roof thrust duplex.
The fault bound bodies of rock in the duplex are called horses.
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.
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Depending on the final orientations of the imbricate faults and the final position of the branch lines a duplex may be hinterland dipping foreland dipping or an antiformal stack.
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.
Duplex is a thrust sheet mass which is bounded by a fioor thrust and a roof thrust often duplex structures are imbricated.
Sole thrust at the base and by a roof thrust at the top mcclay 1992.
A duplex as a reminder is an array of thrust horses bounded by a floor thrust i e.
Else in the world.
A dictionary of earth sciences dictionary.
The rock masses bounded by these faults are calledhorses and the entire structural association is a duplex.
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.
Two flat segments called thefloor and roof thrusts connected by several parallel ramp segments.
Also upper and lower detachments have been described in a similar context for fold duplex structures dahlstrom 1969a.
Blind thrusts are those below the erosion surface but their presence is indicated by shortening in the overlying sequence which is achieved by disharmonic.
A duplex consists of a series of imbricate faults that are asymptotic to a roof thrust and a floor thrust.
Boyer and elliott 1982 state that the roof thrust of a duplex is initiated as a major thrust.
In this setting the roof sequence frequently develops passive roof duplexes banks and warburton 1986.
In a thrust envi ronment the structural association is.