Earthquakes triggered by fluid diffusion and boosted by fault reactivation in Weiyuan, China due to hydraulic fracturing
Published: 5 August 2021| Version 2 | DOI: 10.17632/dzz9n6zc2c.2
Contributors:
Minhan Sheng, Risheng Chu, Zhigang Peng, Zigen Wei, Xiangfang Zeng, Qingdong Wang, Yong WangDescription
The dataset contains two files: absolute_location_phase.dat for P-wave arrival times from the REST method and hypoDD_relocation.dat for relocated earthquake hypocenters.
Files
Steps to reproduce
The arrival-time data are generated from the REST method, whereas the refined relocation are produced from hypoDD algorithm. Detail about this dataset can be found in our manuscript submitted to JGR.
Institutions
Georgia Institute of Technology, Chinese Academy of Sciences Innovation Academy for Precision Measurement Science and Technology, University of the Chinese Academy of Sciences
Categories
Earthquake