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We propose a conceptual model of fault nucleation and development.
Caine et al. (1996) proposed a conceptual model of fault zone architecture and related permeability structure that consists of three components: the fault core, a damaged zone, and the protolith.
A three-dimensional statistical model of fault damage zone architecture, incorporating fault size, orientation and spatial characteristics observed in natural examples, is used with a two-dimensional discrete fault flow model to investigate fluid flow and up-scaling of permeability in fault damage zones with a permeability contrast between rock matrix and fault rock of four orders of magnitude.
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A model of fault-tolerance is presented in (Ozaki et al. 2006), which designates multiple actors to each sensor and multiple sensors to each actor to guarantee event notification.
We use a kinematic model of fault-propagation folding above a blind extensional fault, together with a sedimentary model of coarse-grained clastic deposition, to investigate growth-strata geometries associated with fault-tip monoclines.
3D model of faults is built by selecting minimum curvature interpolation, which can reflect 3D spatial distribution characteristics and combination features of faults.
We here demonstrate a simple mechanical model of faulting in elastic half-space from Okada (1992) with several constraints from field observations and estimated fault dip at depth.
The results may also help to further constrain models of fault evolution.
Other RBAC fault models could be used in this experiment, such as malicious faults (Masood et al. 2009) and probabilistic models of fault coverage (Masood et al. 2010).
The modelling of fault ruptures includes two aspects: (1) An individual fault can be triggered by pressure changes associated with fluid injection.
Hence, determination of in situ stresses and modelling of fault stability are essential prerequisites for the safe engineering of subsurface CO2 injection and the modelling of storage capacity.
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