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We use the maximum fault length and the maximum slip rate listed in Kumamoto (1997).
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There is a real chance of a deceptive fracture pattern if: i) the angular values at the intersection of the fault and its fractures (mode I opening fracture) exceed 50° in the wall damage zone; ii) the scaling relation between fault length and maximum fracture length does not fit a power law; iii) fractures acted as shear fractures.
It also provides the ability to set a maximum number of jobs per schedule and a maximum shift length.
Adopting the empirical relation of fault length and maximum displacement by Matsuda (1975), ~6-km-long Suizenji fault zone could have brought ~0.5-m vertical displacement.
Region of sweep shadow is largest when the fault length is larger and angle with doublet well connector is maximum (i.e., 90°).
The amount of slip in each earthquake on the Firouzkuh fault is difficult to estimate, but assuming the entire ∼55 km fault length ruptures in each event, they will have had a maximum magnitude of 7.1.
The total surface rupture length of about 28 km, the maximum slip of 220 cm, and the mainshock magnitude of M J 7.3 are all broadly consistent with the fault length, slip, and earthquake magnitude assigned to the Futagawa segment by the ERC, HERP (2013) based upon the length of the segment.
This observation affects the various faulting parameters which include fault length, width, depth and average slip.
Consequently, the fault length could not be determined (Fig. 3).
b Scaling relationships between fault area (solid line), fault length (dashed line), fault width (dotted line), and earthquake magnitude.
The 'Fault factor' combines the two aforementioned inputs FLF and FT with the fault length (FL).
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CEO of Professional Science Editing for Scientists @ prosciediting.com