The results indicate that the seismicity of the Anninghe-Zemuhe fault zone has always been stronger than that of the Daliangshan fault zone in history, which is consistent with the results from the active fault and paleoearthquake studies.

At the end of Tertiary, hydrocarbons migrated vertically upward from the upper mantle along large fracture belts and accumulated in the porous-fractured reservoirs in the basement and sedimentary cove.

Late Quaternary kinematic characteristic of the back range faults at the Middle Longmenshan fault zone;

Layout parameter determination in buried-hill fractured zone based on forward modeling.;

Analysis on horizontal deformation of Shanxi rift zone in recent years;