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A displacement of maxima will correspond to the dip orientation.
Relationships between several environmental factors (e.g. bedrock classes, surface deposits, elevation, slope, aspect, dip, dip orientation and relation between dip and slope) and land use changes were appraised.
If the slope angle of the initial surface was greater than 7°, the compression induced only one group of thrusts with a dip orientation contrary to the original compression direction.
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The results show that if the initial surface was horizontal or the slope angle was smaller than 7°, the compression induced two groups of thrusts with opposite dip orientations.
Six sets of discontinuities common to all sites were identified and statistically characterised (dip, strike, orientation, density, size, and estimated transmissivity).
Object dip and orientation was measured with a Brunton compass.
The obtained displacement field is consistent with a right-lateral motion along the Hinagu fault, and thus, the rake was assumed to be a right-lateral with no constraint on dip-slip orientation.
Experiments were conducted with the 2D model oriented in the horizontal plane and compared to experiments at the 15° and 30° dip-angle orientations.
The minimum compression σ3 is almost subvertical to the slab orientation (dip ∼ 71°) (Fig. 3).
Related parameters of sine curve are analyzed and converted into the parameters of structure plane, such as the central position, orientation, dip angle and fracture width of structural planes.
It is found that the proposed axial effective thermal conductivity is a function of geometrical parameters of dual-porosity media, such as the porosities (ϕm,ϕf), fractal dimensions (Df,Dl) for porous matrix and fractured network, tortousity fractal dimension (DT), and fracture orientation (dip θ, azimuth α).
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