linguistic:voice_change, quality:corruption, structural:summarization
Tectonic setting

Huaxian lies within the Weihe Basin, one of the rift basins that form the southern and eastern boundaries of the Ordos Block. To the east the basin is continuous with the Shanxi Rift System. The Weihe basin formed during the Paleogene in response to northwest–southeast directed extension. Following a tectonically quiet period during the late Paleogene the rift basins became active again in the Neogene in response to NNW–SSE directed extension, activity that continues to the present. The basins in the Weihe-Shanxi Rift System are bounded by large normal faults, which have been responsible for large historical earthquakes. The Weihe Basin has an overall half-graben geometry, with the main controlling faults, such as the Huashan Fault and North Qinling Fault, forming the southern boundary.