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Geomechanical Modeling of Stress and Fracture Distribution during Contractional Fault Related Folding

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Figure

Figure 1. Maps show the elementary structural features of the Kuqa Depression (a) Location of the study area in the Kuqa De-Structural map of the top Palaeogene in the D gas field, with strikes of fractures obtained from orientated cores by means of the pr
Figure 2. Sketch map showing the restoration of the D fault-propagation fold.
Figure 3. Types of tectonic fractures (a) and statistics of fracture linear density (b) ob-served in the drilling cores and interpreted by imaging logging (FMI)
Figure 4. In-situ stress coordinate system representing fracture distribution and differen-pendicular to σtial stress based on REV
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