“…Besides direct observations in neighboring wells [7], microseismicity [8][9][10][11], tilt mapping [7], treatment pressure analysis [7], production data [7], and reservoir modeling [13] from hydraulic fracturing treatments in many geological environments also support the observation of complex fracture network development at macro scale. The most important natural factors triggering hydraulic fracture complexity were found to be discontinuities (joints, faults, bedding planes) and heterogeneities within the rock mass [3] in conjunction with the in-situ stress field (e.g.…”