Faults (dip and strike, master fault, antithetic fault and synthetic fault).
In input 3D cube data, following results have been determined with the help of time structure maps, coherent maps, time-thickness maps, amplitude maps, amplitude window map and contour maps; Faults (dip and strike, master fault, antithetic fault and synthetic fault).
For example, the Carnaubais fault, the master fault of the rift system, represents the reactivation of the Portalegre shear zone, the major tectonic boundary between Precambrian terrains in the crystalline basement.
The structural features include antiform and a set of extensional faults with master, antithetic and synthetic faults with opposite sense of shear (dip direction and angle ~60°).
That sketch is just one of 79 16th-century Florentine works, shaped into a thematic exhibition that would give even the fault-finding master scant cause for complaint.
As observed in previous modelling studies, our centrifuge experiments suggest that the angle of offset between the master fault segments is one of the most important parameters controlling the architecture of pull-apart basins: the basins are lozenge shaped in the case of underlapping master faults, lazy-Z shaped in case of neutral offset and rhomboidal shaped for overlapping master faults.
The Cataclastic Unit 1 forms a ∼40 m thick band lining the master fault and recording in-situ shattering due to the propagation of multiple seismic ruptures.
In the studied area, the master fault of the VCFZ dips N210/54° and juxtaposes Quaternary colluvial deposits in the hangingwall with cataclastic dolostones in the footwall.
Like home renovators who overhaul the kitchen only to then find fault with the master bath, some dermatology patients feel that, once their wrinkles are relaxed and their brown spots treated, their pores stand out.
Therefore, the present geometry is different from that of other fault-bounded Quaternary depressions of the central Apennines (typically half-graben basins), showing the maximum depth of the substratum in the area close to the master fault.
Here, we propose that the NW SE-trending El MaNW SE-trendingín linElManzano Liued in the northern termination of the Sierra Azul, refleCullíne presence of a halineament master faulocatedhe subsurface.
