Pure and Applied Geophysics

, Volume 176, Issue 12, pp 5279–5289 | Cite as

Long-term In Situ Permeability Variations of an Active Fault Zone in the Interseismic Period

  • Yuchuan MaEmail author
  • Guangcai Wang
  • Rui Yan
  • Bo Wang


Hydraulic properties were estimated by analyzing the continuous water level response to Earth tides in a well intersecting the Qujiang active fault (in Yunnan, China) which had ruptured during the 1970 Tonghai Ms 7.8 earthquake. The in situ permeability from 2001 to 2018 fluctuates around 4 × 10−14 m2, with a variation of about 25%, and the hydraulic diffusivity varies from 0.29 to 0.55 m2/s. The permeability is comparable to the permeability estimated from the slug tests. According to the results, we suggest that the permeability in the damage zone of the Qujiang fault is dynamic, and the fault zone provides a localized horizontal conduit for the along-fault fluid flow. Furthermore, the shallow part of the Qujiang fault may heal incompletely or not heal after the Tonghai earthquake, and the fault may be stable between 2001 and 2018.


Permeability fault zone well water level tidal analysis Tonghai earthquake 



The water level data, earthquake catalog, and meteorological data were obtained from the China Earthquake Networks Center. This research work was supported by the National Natural Science Foundation of China (U1602233), the National Key R&D Program of China (2018YFC1503305), and the Spark Program of Earthquake Science of China (XH19055). We are grateful to Dr. Giuliana Rossi and an anonymous reviewer for their helpful comments and suggestions.


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Copyright information

© Springer Nature Switzerland AG 2019

Authors and Affiliations

  1. 1.School of Water Resources and EnvironmentChina University of GeosciencesBeijingChina
  2. 2.China Earthquake Networks CenterBeijingChina

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