“…The principle behind the ASR method is that time-independent elastic strain is released first instantaneously, followed by a more gradual or time-dependent recovering of anelastic strain, also called "relaxation", after a rock core is drilled out (e.g., Matsuki, 2008;Gao et al, 2014). The ASR stress measurement takes advantages of the time-dependent strain and of a three-dimensional method, and has been successfully applied in several IODP expeditions (e.g., Byrne et al, 2009;Yamamoto et al, 2013;Oohashi et al, 2017) and other drilling projects (e.g., Matsuki and Takeuchi, 1993;Lin et al, 2006Lin et al, , 2007Cui et al, 2014;Nagano et al, 2015;Sun et al, 2017;Zhang et al, 2022). Here, to determine three-dimensional stress states both above and below the plate boundary fault after the Tohoku earthquake, we collected four whole-round core samples from site C0019 of JFAST and conducted stress measurements by the ASR method onboard D/V Chikyu.…”