“…This paper, however, also stated that earlier work found orientations dependent on the unique stress profiles and rock fabric of a given location (Walker et al, 2002). Coupled flow-geomechanical modeling (Kim and Moridis, 2012) found inherent physical limitations to the extent of fracture propagation-for example, the presence of overlying confining formations may slow or stop fracture growth in the vertical direction, thus containing fractures within the reservoir (Kim et al, 2014). Likewise, find that the majority of induced fractures (with data focused on high-volume fracturing operations in the Barnett Shale in Texas) range from less than 100 m (330 ft) to about 600 m (2,000 ft) in vertical extent, with approximately a 1% probability of a fracture extending 350 m (1,100 ft) vertically.…”