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The ratio of horizontal to vertical displacement across the fault, calculated from the cumulative displacement of landscape features, is 7.6.
Fig. 5 Contours of equilibrium grain size distribution as a function of depth and distance from the fault, calculated from model W1E (a) and D1E (b).
Based on the strain and stress rates of Sumatra Fault calculated from the GPS measurements in Indonesia and its close vicinity, Aydan (2008) predicted an earthquake of magnitude 8.7 in the offshore area of Siberut and Sipora islands, with a rupture length of 400 450 km and an epicentre about 260 km away from the west coast of Sumatra.
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In these geodetic inversions, all authors used the Green's functions (GFs, i.e., theoretical ground surface displacements due to unit dislocations on subsurface faults) calculated for a homogeneous elastic half-space or for horizontally layered elastic media.
Since fracture intensity and apertures in Cleebourg increase towards the fault plane, calculated fracture permeabilities follow this same trend.
The methodology utilizes fault slips calculated from interpreted faults and horizons on 3D seismic to restore the initial state of the rock body in question while considering geomechanical properties, then forward modelling and calculating the paleostresses resulted from various tectonic events.
It is observed that unlike the binary alloy system, the stacking fault probability calculated from peak shift analysis is almost constant with increase in zinc concentration from 10to2020 wt.% and thereafter increases with the increase of zinc concentration.
The activity rate of the main secondary oil source faults was calculated using the fault activity rate method (Table 3).
The amount of shift necessary to correct the fault is calculated from β ( i ) = 1 2 N t ∑ t B ( i, t ) - B ( i - k 1, t ) + ∑ t B ( i, t ) - B ( i + k 2, t ), (9).
For the megathrust fault model, a rupture along a 440-km × 120-km fault is calculated to have almost 3.5 m of slip and will generate a Mw8.5 earthquake.
The pore pressure ratio for each earthquake fault was calculated under the assumption that reduced frictional strength was caused by pore fluid pressure.
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