A structural model is an important part of the geotechnical model of a mine development. The purpose of the structural model is to illustrate the location, orientation and character of major geologic structures, as well as identify the spatial distribution of features that make up the rock mass fabric (i.e minor faults, folds, foliation). The identification of patterns or spatial trends in rock mass fabric allows the selection of structural domains.  Developing domains simplifies the structural evaluation of the block to be mined, by illustrating the interaction of major structures and rock fabric, which may derive a particular overall stress state within that block.  Comprehensive structural evaluation includes geologic structures at all scales – regional mine scale to drill core scale – with enough detail to produce a representative model that reflects the mining block’s entire geological history, formally referred to as tectonogenesis (Figure 1). Illustrating a block’s structural features and unique fault-related movement data contributes to paleostress analysis methods by identifying the controlling structural features and associated stresses. Completing a sequenced paleostress analysis as a means to back-calculate stress through geological time is of significant value to mine sequence planning. This allows assessment of the possibility of remobilizing old structures or veins, resulting in a fault-slip burst or seismic event during mining. Paleostress analysis methods are recommended to be applied at all burst or seismic event prone mine-sites. Using the paleostress back-analysis to estimate the state of stress yields invaluable data for helping develop efficient and safe excavation sequencing during mine-planning. 
Figure 1: Block model reconstruction of geological history and associated paleostress inversion analysis results for inferred stress states based on evaluation of fault slip data. 
Tectonogenesis Assessment and Palinspastic Reconstruction
Tectonogenesis is the unraveling of a block’s geologic tectonic history. Palinspastic reconstruction is the recreation of geo-historical depositional geologic events and kinematic influences. Coupling these together allows the identification of the most influential and controlling structural features of a mining area, which plays a significant role in stability analysis. In the past, tectonogenesis and palinspastic reconstruction have been commonly used for the resolution of geologic history within the petroleum industry, locating oil reservoirs within structurally complex geology. With sufficient research and funding in this particular industry, numerical methods have been established, allowing more rigorous modeling. This rigorous numerical modeling, however, is only effective with good understanding of the area that is being modeled, further necessitating the procedure of tectonogenesis and palinspastic reconstruction. The following steps are recommended to complete a tectogenetic assessment:
- Literature review of the area for regional and local geology, including surface geologic mapping
- Establish the chronological sequence of tectonic events, and regional and local scale deformation (i.e. faulting).
- Examine available drill core with particular attention paid to major structural feature intersections with the drill holes
- Modeling in three-dimensions the identified drill hole intersections with major structural features, and possibly project them in 3D space relative to the geological model.
- Display structural data representing rock mass fabric and major structures on stereonets to define structural domains at the regional scale.
- Isolate block models and domain stereonets to define the sequence of events at the various scales.
- Link, where possible, inferred structural paleostress with principal ground stresses. This will be a preliminary estimate until mining occurs and stress measurements are collected.
The goal of paleostress analysis is to derive the direction of slip on a fault, using basic fault data collected in the field. There are many methods of paleostress inversion, which outline different approaches to the problem, however they are all based on similar assumptions:
- Slip on a fault plane occurs in the direction of the resolved shear stress
- Individual faults do not interact – movement on one fault is independent of another
- The blocks bounded by the fault planes do not rotate
- The stress field activating the faults is time-dependent and homogeneous
Data pertaining to a particular fault includes the fault plane orientation, slip direction and sense of slip, as well as location and character of fault attributes, the sense of slip also referred to as striations, indicate the direction of fault movement (Figure 2). 
Figure 2: Fault data pertaining to the paleostress tensor. 
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