The rupture propagated along the dip direction, and the maximum slip occurred at the hypocenter.
Zhang Lifen, Iman Fatchurochman, Liao Wulin, Li Jinggang, Wang Qiuliang 2013, 'Source rupture process inversion of the 2013 Lushan earthquake, China', Geodesy and Geodynamicshttp://www.sciencedirect.com/science/article/pii/S1674984715300707. Retrieved from DOAJ CC BY 4.0 (https://creativecommons.org/licenses/by-sa/4.0/legalcode)
And the difference of hypocenter mechanism between hydraulically connected and unconnected regions was further discussed.
Xinfang MA, Ning LI, Congbin YIN, Yanchao LI, Yushi ZOU, Shan WU, Feng HE, XiaoqiongWANG, Tong ZHOU 2017, 'Hydraulic fracture propagation geometry and acoustic emission interpretation: A casestudy of Silurian Longmaxi Formation shale in Sichuan Basin, SW China', Petroleum Exploration and Developmenthttp://www.sciencedirect.com/science/article/pii/S1876380417301167. Retrieved from DOAJ CC BY 4.0 (https://creativecommons.org/licenses/by-sa/4.0/legalcode)
For determination of hypocenter location probability density function was used.
Eryk Święch, Paweł Wandycz 2015, 'Differences between downhole and surface micro-seismic monitoring', Mining Sciencehttp://www.journalssystem.com/ms/DIFFERENCES-BETWEEN-DOWNHOLE-AND-SURFACE-MICRO-SEISMIC-MONITORING,60952,0,2.html. Retrieved from DOAJ CC BY 4.0 (https://creativecommons.org/licenses/by-sa/4.0/legalcode)