Roof Thrust Duplex

Duplex is a thrust sheet mass which is bounded by a fioor thrust and a roof thrust often duplex structures are imbricated.

Roof thrust duplex.

The rock masses bounded by these faults are calledhorses and the entire structural association is a duplex. Sole thrust at the base and by a roof thrust at the top mcclay 1992. 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. 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.

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. Else in the world. You can also visit the homepage and enjoy the wonderful photographies with very good examples from many places around the planet. Duplexes have a variety of forms and sizes depending on the amount of displacement of the individual horses.

A duplex consists of a series of imbricate faults that are asymptotic to a roof thrust and a floor thrust. In a thrust envi ronment the structural association is. 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. Two flat segments called thefloor and roof thrusts connected by several parallel ramp segments.

A dictionary of earth sciences dictionary. A duplex as a reminder is an array of thrust horses bounded by a floor thrust i e. The fault bound bodies of rock in the duplex are called horses. Also upper and lower detachments have been described in a similar context for fold duplex structures dahlstrom 1969a.

In this setting the roof sequence frequently develops passive roof duplexes banks and warburton 1986. 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. Blind thrusts are those below the erosion surface but their presence is indicated by shortening in the overlying sequence which is achieved by disharmonic.