This tectonic stress field feature is consistent with the basin prototype, basin reversal and tectonization forming in the relevant period.
这种应力场特征与上述阶段形成的盆地原型、盆地反转、构造变形相匹配。
The geothermal anomaly, low velocity zone and high conductivity layer in crust, and frequent occurrence of strong earthquakes show that the study area is an active area of modern tectonization.