Abstract
In the starting area of Xiongan New Area, the high-density resistivity method is used for fine detection of the deep-lying strata 0m ∽ 200m in the study area. The stratigraphic and lithologic framework of 0 m-200 m depth has been established. The results show that the middle and Late Pleistocene strata are rich in fine sand, and no hidden ground fissures have occurred. It is proved that the high-density resistivity method is effective and feasible in urban planning and construction geological exploration, and it can provide data support for the further construction of Xiongan New Area.
Full Text 
Sign-in/Register to access full text options
Sign-in/Register to access full text options 
Published version (
Free)
Free) 
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a call
