Also upper and lower detachments have been described in a similar context for fold duplex structures dahlstrom 1969a.
Roof thrust duplex.
A duplex consists of a series of imbricate faults that are asymptotic to a roof thrust and a floor thrust.
Sole thrust at the base and by a roof thrust at the top mcclay 1992.
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.
The rock masses bounded by these faults are calledhorses and the entire structural association is a duplex.
In this setting the roof sequence frequently develops passive roof duplexes banks and warburton 1986.
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.
Duplexes have a variety of forms and sizes depending on the amount of displacement of the individual horses.
Duplex is a thrust sheet mass which is bounded by a fioor thrust and a roof thrust often duplex structures are imbricated.
A duplex as a reminder is an array of thrust horses bounded by a floor thrust i e.
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.
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.
Boyer and elliott 1982 state that the roof thrust of a duplex is initiated as a major thrust.
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Source for information on roof thrust.
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.
A dictionary of earth sciences dictionary.
In a thrust envi ronment the structural association is.
Two flat segments called thefloor and roof thrusts connected by several parallel ramp segments.